NASA
Conference
Publication
3099
Multisource Data Integration in Remote Sensing
James C. Tilton, Editor Goddard
Space Flight Center Greenbelt, Maryland
Proceedings of a workshop sponsored by the Institute of Electrical and Electronic Engineers (IEEE) and the NASA Goddard Space Flight Center and held at the University of Maryland College Park, Maryland June 14-15, 1990
IW_A National Aeronautics and Space Administration Office of Management Scientific and Technical Information Division 1991
FOREWORD On June 14-15, 1990, Technical Committee 7 (TC7) of the International Association for Pattern Recognition (IAPR) held a Workshop on "Multisource Data Integration in Remote Sensing" in College Park, Maryland. The original plan for this workshop was to place it in between two major, related conferences: the International Geoscience and Remote Sensing Symposium (IGARSS'90) at the end of May 1990, in College Park, MD; and the International Conference on Pattern Recognition (ICPR'90) in mid-June 1990, in Atlantic City, NJ. Such a configuration of two major conferences in geographically and temporally close range would have offered an excellent opportunity to realize a major goal of TC7: to bring together scientists from remote sensing applications and from the methodology of pattern recognition. Due to the postponement of the ICPR'90, the time between the two conferences became too long to allow participants of both conferences to attend the workshop by a short prolongation of their stay in the area. We therefore moved the workshop close to the ICPR to at least partly reach our goal. The subject of the workshop, Multisource Data Integration in Remote Sensing, seems to have become a real challenge for the near future. New instruments and new sensors will provide us with a large variety of new views of the "real world." This huge amount of data has to be combined and integrated in a (computer-)model of this world. But also, the knowledge of how these data are gathered and what their characteristic properties are is among the useful sources of information that contribute to a meaningful interpretation. Multiple sources may give us complementary views of the world -- consistent observations from different (and independent) data sources support each other and increase their credibility, while contradictions that may be caused by noise, errors during processing, or misinterpretations, can be identified as such. As a consequence, data integration can produce results that are very reliable, and represents a valid source of information for any geographical information system (GIS). The workshop structure consisted of three sessions of three to five individual presentations. All papers were discussed both individually and in the general context of the session. Additionally, all papers were considered under four specific aspects: 1. What are the characteristic properties of the data sources that are explored approach? 2. In which category does the used integration method fall? 3. What is the result of the integration and what are the improvements realized? 4. What are the major advantages of the proposed methods?
in the individual
Four participants generously volunteered to consider the papers under one of the above aspects. Started as an experiment to encourage lively discussion, the four summaries (three of which are included herein) prove the success of this approach, and give also a useful index to the presented papers. It was an interesting experience for the authors to get a feedback on their own presentations. Last but not least, I would especially like to thank Dr. James C. Tilton of NASA Goddard Space Flight Center for the excellent organization of this workshop. I would like to further acknowledge the sponsors of the workshop, the IAPR, NASA Goddard Space Flight Center, and the Washington/Northern Virginia Chapter of the IEEE Geoscience and Remote Sensing Society. My thanks go also to the authors that have contributed papers and to all the active participants that made the workshop more than just a sequence of presentations. I hope that activities of IAPR-TC7 will continue in the future under the leadership of the new chairman of TC7, Dr. Tilton, and that we can reassemble for another interesting workshop -- probably in 2 years -- on the occasion of the next ICPR, which will be held in The Hague, The Netherlands. Dr. Walter
G. Kropatsch
,°,
111
PRECEDING
PAGE
BLANK
NOT
FILMED
CONTENTS °oo
Foreword
111
Contents
V
PRESENTATIONS 3
Refinement of Ground Reference Data with Segmented Image Data Jon W. Robinson, ST Systems Corporation, Lanham, MD, USA James C. Tilton, NASA Goddard Space Flight Center, Greenbelt, MD, USA Near Ground Level Sensing for Spatial Analysis of Vegetation John Rasure, Tom Sauer, and Charlie Gage, Department of Electrical and Computer Engineering, University of New Mexico, Albuquerque, NM, USA
11
Integration
of SAR and DEM Data - Geometrical Walter G. Kropatsch, Institute for lnformatics, University Innsbruck, Innsbruck, Austria
27
Towards
Operational Multisensor Data Registration Eric Rignot, Ronald Kwok, and John Curlander, Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA, USA
Considerations
39
Combined Fluorescence, Reflectance, and Ground Measurements of a Stressed Spruce Forest for Forest Damage Assessment C. Banninger, Institute for Image Processing and Computer Graphics, Joanneum Research, Graz, Austria A Phenomenological and Visible Data
Approach
to Multisource
Data
Integration:
Analysing
Norway
Infrared
54
61
N. Nandhakumar, Electrical Engineering Department, University of Virginia, Charlottesville, VA, USA A Method for Classification of Multisource Data using and Its Application to HIRIS Data H. Kim and P. H. Swain, School of Electrical Engineering and Laboratory for Applications of Remote Sensing, Purdue University, West Lafayette, IN, USA
Interval-Valued
Improved
of Monocular
Disparity Map Analysis Through the Fusion Frederic P. Perlant and David M. McKeown, Digital Mapping Laboratory, Carnegie Mellon University, Pittsburgh, PA, USA
v
PRBCEUiNG
Probabilities
83
Segmentations
P,_GE
75
_C,q
F_LMED
Useof InformationFusionto Improvethe Detectionof Man-MadeStructuresin Aerial Imagery
94
Jeffrey Shufeit and David M. McKeown, Digital Mapping Laboratory, Carnegie Mellon University, Pittsburgh, PA, USA A Computer Vision System for the Recognition of Trees A. Pinz, Institute of Surveying and Remote Sensing, University of Agriculture, Wien, Austria
in Aerial
111
Photographs
Visualizing Characteristics of Ocean Data Collected During the Shuttle Imaging Radar-B Experiment David G. Tilley, The Johns Hopkins University Applied Physics Laboratory, Laurel, MD, USA
125
A Proposal to Extend Our Understanding of the Global Economy Robbin R. Hough, Oakland University, Rochester, MI, USA, and Manfred Ehlers, University of Maine, Orono, ME, USA
135
SUMMARIES Summary
of Data Sources Utilized in Workshop Papers James C. Tilton, NASA Goddard Space Flight Center, Greenbelt, MD, USA
Summary
of Types of Data Fusion Methods Utilized in Workshop Sylvia S. Shen, Lockheed Palo Alto Research Lab., Palo Alto, CA, USA
Summary
of Types of Data Output Produced by Studies Described Axel J. Pinz, Institute of Surveying and Remote Sensing, University of Agriculture, Wien, Austria
143
145
Papers
In Workshop
Papers
151
APPENDIX 155 Participants
vi
PRESENTATIONS
N91-15616 Refinement
of Ground
With Segmented Jon W. Robinson Image Analysis Section ST Systems Corporation 4400 Forbes Boulevard Lanham, MD 20706 Phone: (301) 794-5200 E-Mail:
[email protected]
Reference Image
Data
Data
James C. Tilton Mail Code 936 Information Systems Development Facility NASA Goddard Space Flight Center Greenbelt, MD 20771 Phone: (301) 286-9510 E-Mail:
[email protected]
ABSTRACT There are a variety of ways for determining ground reference data for satellite remote sensing data. One of the ways is to photo-interpret low altitude aerial photographs and then digitize the cover types on a digitizing tablet. These digitized cover types are then registered to 7.5 minute U.S.G.S. maps that have themselves been digitized. The resulting ground reference data can then be registered to the satellite image, or, alternatively, the satellite image can be registered to the ground reference data. Unfortunately, there are many opportunities for error when using a digitizing tablet and the resolution of the edges for the ground reference data depends on the spacing of the points selected on the digitizing tablet. One of the consequences of this is that when overlaid on the image, errors and missed detail in the ground reference data become evident. This paper discusses an approach for correcting these errors and adding detail to the ground reference data through the use of a highly interactive, visually oriented process. This process involves the use of overlaid visual displays of the satellite image data, the ground reference data, and a segmentation of the satellite image data. Several prototype programs have been implemented on the VAX computer system and the IVAS image display system to examine various methodologies for improving ground reference data. These programs provide a means of taking a segmented image and using the edges from the reference data to mask out those segment edges that are beyond a certain distance from the reference data edges. Then using the reference data edges as a guide, those segment edges that remain that are judged not to be image versions of the reference edges are manually marked and removed. We describe the prototype programs that were developed and the algorithmic refinements that facilitate execution of this task. Finally, we point out areas for future research.
INTRODUCTION There are many ways to use multiple data sources in remote sensing. In this paper, we discuss a method for using image data to improve ground reference data sets. Reference data sets are sometimes referred to as "ground truth"; however, since the methods of creating reference data sets provide many opportunities for error, we will use the term reference data set. This terminology allows for the possibility of using multiple data sources for determining not only the contents of the reference data set but also for refining it.
This work was supported by the Office NASA Headquarters, Washington, DC.
of Aeronautics,
Exploration
and
Technology,
We have obtained
satellite image data from a number of investigators along with reference data sets that they created. By using the image data to create a segmented image, edges consistent with the spectral variation in the image are created. Visual inspection of the reference data edge map overlaid on the raw image or the segmented image reveals many discrepancies. These may be errors, or simply inappropriate attention to detail by the person generating the reference data (particularly if they were digitizing data from a digitizing tablet). An example exhibiting displacement errors and too coarse of a digitization scale is given in Figure 1. While it would be desirable to have an automatic method of using the segmented image data to revise the reference data set, we chose, as a first approximation, to develop prototype methods that allow interactive selection and deletion of the segmented image edges that appeared to be too far from those edges generated from the reference data set. The end result is to leave a set of edges that are considered to be the true edges derived from the segmented image data, based on their proximity to the original reference data set edges. METHODS A series of allowed the attached to a segmentation Processor) at
programs were developed using IDL (Interactive Data Language) that user to use either an IIS system 575 terminal or an IIS IVAS terminal VAX cluster for interactive editing of the edge map generated by an image algorithm (Tilton, 1989) which runs on the MPP (Massively Parallel Goddard Space Flight Center.
The image segmentation algorithm is an iterative process. At each iteration, those regions that are most similar by a particular criteria (e. g., minimum change in image entropy, or minimum rise in image mean squared error) are merged. As the number of iterations increase, the number of image segments decreases. A program called "edge.movie" that runs on the IIS System 575 was developed that allows the user to view various iteration steps and compare these with the original reference data set edges and bands from the image data. This program allows the user to interactively pick an iteration and then immediately compare it with these other sources of information. It is best to select an iteration with more segments and edges than necessary to fit the reference data so that a crucial segment edge that may match a particular reference edge will not be lost. On the other hand, choosing too low an iteration and thus an image with too many segments and edges increases the work load of the analyst significantly. The next step is extract the edges of the selected iteration from the combined edge file which contains the edges from all iterations coded by iteration number. This leaves an image of all of the edges present at iteration n with the pixel value of the edge indicative of its age. The original reference data is a raster format image divided into regions. function, GREFEDGE.PRO was written to extract the edges from this image.
An
IDL
This segmented edge file is then masked with the edge file from the reference data to eliminate all edges that are beyond a specified distance from the reference set edges. This distance is selected by the analyst and depends on the image set being analyzed. Figure 2 shows an example of this process after this masking is complete.
4
Becausethe main algorithm for this procedurecanonly processimagesthat are 128x 128,sectionsof this sizeor smallermustbeextractedfrom larger imagesfor processing andthen be recombinedto producea final product. In orderfor there to be continuity betweensectionsit is necessaryto havea certainamountof overlapbetweenthem. The degreeof overlaprequiredis beinginvestigatedin ongoingstudies. Two programs,CHGVAL5.pro and CHGVAL4.pro (for the IIS System575 and IIS IVAS respectively)werewritten in IDL to provide a prototypeinteractiveenvironment (listings in AppendixA). The input files (image,segmentedge,original referenceedge) for eitherof theseprogramscaneitherbe input oneat a time asthe programrequestsor the input file namescanbereadfrom aninput file. The CHGVAL5.pro programfor the IIS System575 image display systemusesa track ball to movethe cursoron the imagedisplayandthe track ball function buttonsto either deleteanedgepixel, replaceandedgepixel or go on to the next stepin theprogram. The CHGVAL4.pro program for the IIS IVAS systemfunctions the sameway except that it allows the displayto be zoomedandroamedwhenlooking for edgesto delete. In addition,the IIS IVAS systemusesa threebuttonmouseinsteadof a multi-buttontrack ball. The CHGVAL#.pro programsstart by asking whetherthe analystwishes to enter the namesof the imagefiles individually or whetheran input file containingall of the other input items is to be used. Sincethe programis usuallyinvoked manytimes to complete the processingof a singlesection,the useof the input file savesthe analystthe troubleof rememberingandtyping in all of theotherfile nameseachtime the programis usedon a section. The edgesfrom the original referenceimage are loadedinto the graphicsplane of the display device. Two bandsof the original imagedataareloadedinto the red and green display memoriesandthe edgesfrom the maskedsegmentededgeimage areloadedinto theblue displaymemory. In the CHGVAL5.pro programfor the IIS system575,the analystusesthe track ball to movethe cursoroverpansof the blue edgeimagethatthey wish to removeandclick on the appropriatetrack ball button, producing "nicks" in the selectededge. For the CHGVAI.,4.proprogramfor the IIS IVAS system,the usercanzoomandroamthe image with the mousefirst so it is easierto seewhatandwhereoneis deletingedgesegments. The terminalmonitorpromptsthe userwith thecurrentfunctionsof the trackball buttons or the mousebuttons. An exampleof this processafter nicking severaledgesis given in Figure3. After havingnicked a numberof edgesfor removal,the analystcanexit this part of the program and the nicked edgeimage is written out to a file for processingby a batch program that runs on the MPP. After writing out the nicked edge image, the CHGVAL#.pro programsubmitsthe batchprogramto the MPPandwaits for it to finish. The MPP program writes out the new edge image with the nicked edgescompletely removed. The CHGVAL#.proprogramthenreadsin the new edgeimage and writes it out to thered displaymemorysothe analystcanreview theresultsof his work. When the new edgeimage is readinto the red memorybank,thosepartsof the original edgeimagethatweredeletedshowup asblue andthosepartsthat werenot deletedshow up asmagenta(red "newedgeimage"+ blue "blueold edgeimage"). The analystis then given the choiceof undoingsomeof his deletionsor continuing with further nicking or
5
quitting andsavingtheresult. An exampleof the final resultfrom CHGVAL#.PROfor a single128x 128sectionof datais givenin Figure4. There are two types of edge connectivity that can be used, 8 connected and 4 connected. With 8 connected edges, unexpected deletions can chain through edge intersections. Thus it is particularly useful to have a number of ways of back tracking. Our prototype system provides several alternative ways to recover edges. The simplest method is that while nicking lines, the user can undo a nick by placing the cursor over the nicked pixels and pushing the appropriate key on the mouse or the track ball. Alternately, the user can run a test, deleting the nicked edges and determine whether he wants to undo some of the nicks. If the user chooses to undo some of the nicks he can either fill in particular nicks using the cursor control device or he can pop deleted pixels off of the stack into their former locations. The latter method is most effective if the most questionable
deletes
are saved
until near the end of a nicking
cycle.
These methods of recovering erroneously deleted edges only work within a single nick and try cycle. If one either continues with a new nick and try cycle or saves the last result and exits the CHGVAL#.PRO program, then another method must be used to recover lost edges. In order to repair or recover edges after leaving the CHGVAL#.PRO a program that would allow pasting edge pixels from an earlier edge image into the current edge image was developed. This program puts one band of the image into the green display memory, the edge image to be fixed into the blue display memory and the master or original edge image into the red display memory. The user then uses the cursor control device to put the cursor over the master edges that he wishes to copy to the edge image to be fixed and presses the appropriate button. This puts a copy of the master pixel overlayed by the cursor into the edge image to be fixed. In this manner each pixel of an edge segment in the master image can be copied into the edge image to be fixed. An appropriate change in color takes place for each pixel that is moved into the edge image that is being repaired so the user can tell which pixels are present in both images. The above description is summarized in Figures data flow from the original image and ground edges (producing a revised ground reference describing the CHGVAL_.PRO programs. After
several
overlapping
128x128
edge
images
5 and 6. Figure 5 illustrates the overall reference data to the revised reference data file). Figure 6 is a flow chart
have
been
edited,
it is necessary
to
rejoin them into a single image, to delete nonterminating edges in the overlap region and to join edges from overlapping segments. Another IDL procedure, COMBCHG4.PRO that runs on the IIS IVAS display is being developed to accomplish this task. Since its functions are so similar to those of CHGVAL4.PRO it is being designed to perform these functions also. Two test images are being used. The first is a 468 x 368 pixel Thematic Mapper (TM) image of the Ridgely Quadrangle on the eastern shore of Maryland. It contains few classes and most of them are large in area. The main features of the scene are fields and wooded streams. There are small areas of water, ponds, and single urban area. These areas were digitized from a 7.5 United States Geological Survey quadrangle map that had had its reference data boundaries drawn on a plastic overlay from 1977 aerial photographs using a digitizing tablet (Gervin, et al., 1985). In the original study, the ability of AVHRR and MSS data to distinguish Level 1 land cover classes was examined. This involved registering the MSS data to the Ridgely Quadrangle and resampling it to 60 meter pixels. This lead to the ground reference data being rasterized to 60 meter pixels. Since the pixel size of the original reference data set was 60 meters and TM data
6
is 30 meters,the disparity betweenthe TM boundariesandthereferencedataboundaries, andlack of detail in thereferencedataareunderstandable.Examplesshownin Figures1 through4 arefrom a 128x 128sectionin the upperleft comerof this dataset. The secondimageis a portion of the WashingtonD.C. metropolitanarea. This areawas brokendowninto moreclassesthanthe Ridgelyquadrangleandthe classesaresmallerin size. Testswith this datasetwerenot yet completedasof this writing. RESULTS& DISCUSSION In practice, the prototypesworked well, allowing the edge maps to be trimmed by nicking thoseedgesto be deleted. Problemswereprimarily onesof speedin loading the original referencedatainto thegraphicsplane. The useof 8 connectededgeslead to unexpectedchainsof deletions. Becausethis was so severe,the processingprocedureswerestartedoverusing4 connectededges. Joining the segmentswith overlappingboundarieswas not a seriousproblem with the Ridgelyquadrangle.Thelarge areasandconcomitantsmallnumberof edgescontributed to the eachin joining the segmentstogether. Looking again at Figure4, note that refined groundreferenceboundaries(obtainedby selecting boundaries from the image segmentation)follow very closely visible boundariesin the imagedata. In particular,notethevery coarse,misregisteredboundary from the original groundreferencefile the top middle of the image. The refined ground reference boundary is perfectly registered,and follows the actual variations in the boundaryvery closely. We plan to use this and other data setsin comparativestudiesof various algorithms designedto extractspatialinformationfrom imagery. We expectthat therefined ground referencedata will help to more accuratelyevaluatethe behaviorof thesealgorithms thanwould theoften too coarseandmisregisteredoriginal groundreferencedata. REFERENCES Gervin, J. C.,
A. G. Kerber, R. G. Witt, Y. C. Lu and R. Sekhon, 1985, "Comparison of Level I Land Cover Classification Accuracy for MSS and AVHRR Data," International Journal of Remote Sensing, 6(1), pp. 47-57 Tilton, J. C., "Image Segmentation by Iterative Parallel Region Growing and Splitting," Proceedings of the 1989 International Geoscience and Remote Sensing Symposium, Vancouver, BC, Canada, July 10-14, 1989, pp. 2420-2423.
7
=
Figure 1. Edges (black) overlaid Landsat Thematic the displacement scale compared to
Figure 2. Edges from a ground reference file (white) and edges from an image segmentation (gray) overlaid upon the corresponding Landsat TM image. Image segmentation edges further than 6 pixels from a ground reference edge have been masked out.
from a ground reference file upon the corresponding Mapper (TM) image. Note errors and coarse digitization the Landsat data.
Figure 4. Edges from a ground reference file (white) and the final selection of corresponding edges from an image segmentation (gray) overlaid upon the Landsat TM image. This final selection of edges can now be used to generate a label map that can be used as a substitute for the original ground reference file.
Figure 3. Edges from a ground reference file (white) and edges from an image segmentation (gray) overlaid upon the corresponding Landsat TM image. Image segmentation edges that are shown to be "nicked" in this image will be deleted by the next processing step (connected components labeling).
ORTGINAL
8 BLACK
AND
WHITE
PAGE PHOTOGRAPH
ground reference
image]
label
map
SEGMENTATION IMAGE ]
U SELECT ITERATION
EXTRACT EDGES
EXTRACT EDGES
SEGMENT EDGES MASK OUTPP) (GREFMASK.
I segment edges
reference edges
J
masked segment edges
__.___ _-"6 ¢)
A
_! -_
_ ,_ _ .- _ ,,
_-_ _ _o _ ,.
E
0 D
"
N
IJJ ._1 '¢_
E
rr
,,
-,-__
_,
>0
k-.._ 5_
0. "I
57
m
0
,,
58
N91-15620 COMBINED FLUORESCENCE, REFLECTANCE, MEASUREMENTS OF A STRESSED NORWAY FOR
FOREST
DAMAGE
AND GROUND SPRUCE FOREST
ASSESSMENT
C. Banninger Institute
for Image
Processing and Computer Joanneum Research
Wastiangasse Tel. (316) E-Mail:
6, A-8010, 8021, Telefax
Graz,
Graphics,
Austria
(316) 8021-20,
[email protected]
The detection and monitoring of stress and damage in forested areas is of utmost importance to forest managers, who require timely and accurate information on the state of health and vitality of this natural resource for planning purposes. The extensive and often difficult-to-assess nature of many of the world's forested regions makes remote sensing the most suitable means to obtain this information. This requires that remote sensing data employed in a forest survey be properly chosen and utilised for their ability to measure canopy spectral features directly related to key tree and canopy properties that are indicators of forest health and vitality. Plant reflectance in the visible to shortwave infrared regions (400-2500 nm) provides information on its biochemical, biophysical, and morphological make up, whereas plant fluorescence in the 400-750 nm wavelength region is more indicative of the capacity and functioning of its photosynthetic apparatus. A measure of both these spectral properties can be used to provide an accurate assessment of stress or damage within a forest canopy. What is necessary is to define the specific wavelengths within these spectral regions that provide optimal information on a plant's health and vigor. Foliar chlorophyll and nitrogen are essential biochemical constituents required for the proper functioning and maintenance of a plant's biological processes. Chlorophyll-a is the prime reactive centre for photosynthesis, by which a plant converts carbon dioxide and water into necessary plant products. Nitrogen forms an important component of the amino-acids, enzymes, proteins, alkaloids, and cyanogenic compounds that make up a plant, including its pigments. The measurement in a canopy by remote sensing methods would allow the rapid appraisal of a forest's state of health. Both chlorophyll and nitrogen have characteristic absorption features in the visible to shortwave infrared region that furnish information on their content within a canopy. By measuring the wavelength position and depth of these features and the fluorescence response of the foliage, the health and vitality of a canopy can be ascertained. For a stressed Norway spruce forest in southeastern Austria, foliar chlorophyll-a and nitrogen content and leaf area indices (LAD were derived and foliage reflectance and fluorescence measurements obtained from samples collected at 50-m grid intervals over the test site. The discrete data sets were transformed into continuum data sets in the form of isopleth maps, and resolution cells corresponding to the size of the ground-projected pixels of the Landsat Multispectral Scanner (MSS) and Thematic Mapper (TM), NS001 Thematic Mapper Simulator (TMS), Thermal Infrared Multispectral Scanner (TIMS), Airborne Imaging Spectrometer (AIS-2), and Fluorescence Line Imager/Programmable Multispectral Imager (FLS/PMI) sensor systems derived for each ground data set. These cellularised data sets served as the reference data for evaluating the capabilities of the various remote sensing data used to differentiate stress or damage in the test site forest, which served as a test model for the development of remote sensing-based algorithms for more universal application. In addition to chlorophyll-a, nitrogen, and LAI data, other canopy biochemical constituents, canopy biogeochemistry, soil geochemistry, and site slope, aspect, and elevation information has been incorporated into the cell data bases. Examples of these will be presented in the paper.
59
N91-15621 A
Phenomenological Analysing
Approach Infrared
to
Multisource and Visible
Data Data
Integration:
N. Nandhakumar Electrical
Engineering
Dept.,
Univ.
of Virginia,
Charlottesville,
VA 22903
Abstract A new method is described approach uses phenomenological are based on intrinsic analyzed to estimate
for combining multisensory data for remote sensing applications. models which allow the specification of discriminatory features
physical properties surface heat fluxes.
of imaged surfaces. Thermal and visual images Such analysis makes available a discriminatory
is closely related to the thermal capacitance for labelling image regions based on physical from existing approaches which nonlinear combination of signal evidential approach.
1
of the imaged objects. This properties of imaged objects.
The that
of scenes are feature that
feature provides This approach
a method is different
use the signal intensities in each channel (or an arbitrary linear intensities) as features - which are then classified by a statistical
or or
Introduction
Multispectral/multisource riety of applications such
data acquired via remote sensing have been shown to be useful for a vaas urban land-cover assessment, rain-rate classification, crop assessment,
geophysical investigation, and surveillance and monitoring for national defence techniques have been developed for combining the information in the different These techniques typically use statistical or evidential rules to achieve the desired The
usual
statistical
approach
consists
of first
forming
a feature
vector
activities. Various sensing modalities. classification.
wherein
each
element
corresponds to the signal value (pixel gray level) from each sensor. This feature vector is then classified by a statistical decision rule. Other features such as the mean intensity level in a beighborhood, contrast, second and higher order moments, entropy measures, etc. have also been used as elements of the fusion
feature vector, of information
e.g. [1]. In such approaches, interpretation of the imaged scene based on the from the different sensors may be said to occur at the lower levels of analysis.
In some techniques, linear and/or nonlinear combinations of signal values from different sensors form a feature, several of which are then fed to a classifier, e.g. [2]. In the latter case, interpretation may be said to occur at higher levels of analysis, after an earlier stage of information fusion which extracts discriminatory
features.
Other
extensions
to the standard
statistical
approach
have
been
reported,
e.g., a fuzzy relaxation labelling approach for image interpretation has been reported [3] wherein a Gaussian maximum likelihood classifier is used to provide initial probability estimates to the relaxation process. Different optimal classification rules have been developed for interpreting multisource data each of a variety of statistical models assumed for the data. The classifiers however do not address problem
of choosing
sufficiently
Such approaches therefore is impossible to guarantee.
sets are warranted for achieving of the imaged objects are being Evidential
approaches
discriminatory
features
from the infinite
number
of available
suffer from the disadvantage that the global optimality Also, training of such classifiers is difficult since very a reasonable error rate. It is also not clear what utilized by the classifier during the discrimination
have also been
developed
61 PRL:=CEDiNGPAGE I_LAhlK NOT FILMED
for combining
information
for the
features.
of the feature set large training data physical process.
properties
from multiple
sensing
i T.erma,,mage I I V sua,,ma0e 1 Surface Temperature _irVe_city
Jf
I
Air_mp.
Radiated Convected Heat HeatFlux Flux '
I Surface Reflectance, Orientation
I
Date, Time_,l
I I Absorbed HeatF,ux I •
i
I Conducted
i
Heat Flux
I
I Temp.
I
R = Conducted/Absorbed I
Figure
1. Combining
thermal
modalities, e.g. [4]- [6]. Such methods contrast measures for each sensor and
Region Labels
and visible
data
I
Refl.
l
for surface
heat
rely on a large set of heuristics compare outputs from different
flux estimation.
rules which examine local sensors to provide varying
degrees of support (certainty values) for a hypothesized class. A non-probabilistic framework is used for updating these uncertainties to reach a final classification. Interpretation in such systems is attempted at multiple levels of analysis. The rules, however, are based on manifestations of the differences in the intrinsic physical properties of objects rather than on direct measures of the physical properties themselves. fusion.
in multisensor
data
Due to these reasons, it is desirable to first combine information from the different sensors on a physical model of the scene with the objective of evaluating intrinsic physical properties
based of the
imaged features higher
Such approaches
therefore
do not fully exploit
objects. Such an a_alysis allows for specification which may then be used for scene interpretation
the synergy
available
of physically meaningful and discriminatory by a probabilistic or evidential classifier at
levels of analysis.
This paper discusses the development fusion of information from infrared (IR) which principles of heat transfer sinks and sources in the scene.
and use of phenomenological scene-sensor and visible data. A computational model
models for the is established in
are used along with computer vision techniques to derive a map of heat The approach uses infrared imagery sensed in the 8pro - 12#m band,
monochrome visual imagery, and knowledge of ambient conditions at the imaged surface to estimate surface heat fluxes in the scene. A feature which quantifies the surface's ability to sink/source heat radiation is derived and is shown to be useful in discriminating between different types of material classes
such as vegetation
It is assumed algorithm processed
that
and pavement.
the thermal
image
is segmented
into dosed
regions
by a suitable
segmentation
(e.g., [7]) and that the thermal and visual images are registered. The thermal image to yield estimates of object surface temperature. This process requires the formulation
an appropriate model which relates scene radiosity to surface temperature, the thermal camera to scene radiosity. Several object and scene parameters 62
is of
and received irradiation at such as surface reflectivity,
emissivity,reflectedsceneradiosityareincorporatedin the model.The visualimage,whichis spatially registeredwith the thermalimage,yieldsinformationregardingthe relativesurfaceorientationof the imagedobject. The Lambertianreflectancemodelis usedalongwith the shape-from-shading principle for this purpose.The aboveinformationalongwith informationregardingambienttemperature,wind speed,and the date and time of image acquisitionis usedin a computationalmodel that allows estimationof surfaceheatfluxesin the scene.The estimatedsurfaceheat fluxesareusedto evaluate a featurethat is closelyrelated to the lumpedthermal capacitanceof the object. This featureis shownto bea meaningfulanddiscriminatoryfeaturefor sceneinterpretation.A blockdiagramof the approachis shownin figure 1. Multisensoryimages,andin particular - thermal andvisual images,havebeenusedin the past for evaluatinga rough estimateof thermalinertia for variousremotesensingapplications[8] - [10]. The previouslydevelopedmethodsusevery simplemodelsof the sceneand of the energyexchange phenomena ocurringat the imagedscene.In contrastto thesepastapproaches, the techniquedeveloped in this paperis basedon an explicit andmoredetailedphysicalmodelof the energyexchangein the sceneand providesmoremeaningfulanddiscriminatoryfeaturesfor classification. The remainderof this paperis organizedasfollows.Section2 describesan approachfor extracting accuratesurfacetemperatureestimatesfrom infrared imagery.Section3 discussesthe computation of relative surfaceorientationfrom visual imagery.Section4 describes the estimation of surface heat fluxes at the imaged scene. Section 5 discusses two different ways of using the surface heat flux estimates for scene interpretation. Section 6 presents experimental results using real data, and section 7 contains
2
a summary
of the ideas presented
Estimating
A quantitative
Temperature model
in this paper.
from
has been derived
Thermal
for estimating
Images
the surface
temperature
of a viewed
object
using
the thermal image. Details of the derivation may be found in reference [11]. The salient points of this model are presented below. The model is based on observations that are unique to the situation where outdoor scenes are illuminated by solar radiation. The derivation of the model rests on the following observations and results: 1. Most surfaces
found
in outdoor
scenes may be considered
to be diffuse emitters
in the 8#m-12#m
band. Furthermore, they possess high emissivities in this band - in the range of 0.82 to 0.96. Hence, a constant value of 0.9 may be assumed for the IR emissivity of all imaged surfaces in outdoor scenes. 2. The radiosity radiation, contribute
of an object's
suface
in a natural
scene comprises
and reflection of radiation that emanates to the total irradiation at the IR detector.
the 8#m - 12Ftrn band. the other hand, a large
Foc between
involves
reflected
solar
lie typically between 250K and 350K. Since IR emissivities are at the IR detector is dominated by emission from the surface of
the imaged object. The components other objects may be safely ignored.
and typically
emission,
Furthermore, the surface reflectivities to IR radiation are very low. On percentage of emission from scene objects lies in the 8#m - 12#m band
since their surface temperatures also high the scene irradiation
3. The view factor
surface
from other surfaces. These components Only 0.1% of the total solar energy lies in
due to reflected
the camera
the evaluation
and
imaged
of complex
53
solar radiation
surface
integrals
and reflected
depends
emissions
on the viewing
[12]. A reasonable
from
geometry
approximation
to
d
Ao
Figure 2. View factor between camera and imaged surface. Ac is the circular viewing surface of the detector, _ac is the solid angle subtended by the detector, Ao is projection of A_ onto the imaged surface, d is the distance between the camera and the imaged surface, and 0¢ is the angle between the surface
normal
and
the viewing
direction.
Foc is arrived at by making the following observations. Since the solid angle detector w_ is usually very small (on the order of 2 mrad) we can approximate
subtended by the the projection of
the detector's
patch,
Ao in figure
viewing
surface
onto the imaged
surface
to be a planar
circular
denoted
by
2.
The approximations indicated above allow for the derivation of a simple model that relates the surface temperature of the imaged object to the digitized value of the IR sensor's signal due to irradiation
at the sensor
[11]. The
0.9
resulting
model
is expressed
1 )_s(exp(C-_*_T)
as:
- 1) dA = K_,Lt + Kb
where, C1 and C2 are constants in Planck's equation and and C2 = 1.439 × 104 #inK. T is the surface temperature
(1)
have values: C1 = 3.742 × 10 s W#m/m 2 of the imaged object, )_ is the wavelength
of energy, )q = 8#ra and )_2 = 12#m. Lt is the pixel gray level value of the digitized thermal Ka and Kb are constants for a particular imaging setup and are obtained by appropriate calibration as described below. The
model
established
above
provides
image. camera
a simple
algorithm for surface temperature estimation. At el is created for different values of T; _5(_xp(V_/_T,)_l)d)t
the outset a table of values of F(Ti) = 0.9 f_/ via numerical integration of this expression. A scene
containing
two objects
at two different
known
temperatures is imaged. The corresponding gray level values are used in equation (1) to solve for the constants Ka and Kb. Thereafter, the temperature of other surfaces in other scenes can be determined by first evaluating the right-hand side of equation (1) using the corresponding gray level. Then the table
of values
index
Ti now provides
of F(Ti)
created the surface
above is looked temperature
up for a matching estimate.
54
value.
The value
of the associated
In general,
an exact
match
will not be found
acquire a reasonably accurate value Lt in the thermal image side of equation values of F(T_) F(Tm)
(1) evaluate assume that
< G < F(Tn).
The
has been
desired
value of surface
2. The distance between 3. The
spheric
3
the surfaces
distance
hundred If neither
between
as follows
to
gray level right-hand
for a match in the table of F(Tm) and F(Tn) such that computed
as:
the effect of atmospheric
imaging
appear
in the same
and the thermal
and
the
attenuation
situations:
camera
are to be estimated
surfaces
(2)
thermal
and
camera
scene
that
was used
is the same as the distance
the camera. is on the
order
of only a few
[13].
of the above attenuation
estimation,
surfaces
temperatures
imaged
is then
are to be estimated
the calibration
between
meters
is performed
Tn -Tm (G - F(Tm)) F(T.)- F(T )
for the following
temperatures
whose
temperature
for temperature
This is justifiable
1. The surfaces whose for calibration.
interpolation
to G, i.e., G = K_Lt + Kb. On searching G is found to lie between adjacent entries
the above approach
ignored.
a linear
estimate of the surface temperature. Consider a particular which corresponds to a surface temperature of Ts. Let the
T, = Tm + In deriving
and
conditions
apply,
appropriate
models
need to be applied
to account
for atmo-
loss [13]-[15].
Inferring
Surface
Reflectivity
and
Relative
Orientation
In order to estimate heat fluxes it is necessary above but also surface reflectance to visible
to estimate not only surface temperature as described radiation and also surface orientation relative to the
incident (solar) In the following
of the scene provides clues to both these quantities. the infrared and visual images of a scene are spatially
registered,
radiation. discussion
and that
The visual image it is assumed that
the images
are segmented
a priori into regions
by a method
such as that
described
addressed
by several
in [7]. The
use of shading
information
researchers, e.g. [16]-[20]. satisfied. The bi-directional Image
resolution
to recover
the shape
of an object
has been
These techniques, however, can be applied only if certain conditions are reflectance distribution function of the surface must be known a priori.
must be high enough
to allow the rendition
of several
surface
patches
near the occlud-
ing boundary, or there need to exist background patches of known surface orientation surrounding the region of unknown surface orientation. These conditions are difficult to satisfy when imaging objects in a natural scene. We also note that while the aforesaid efforts attempt the problem of determining the (x, y, z) direction cosines of the surface normals of the imaged surface, our problem is a much simpler one, i.e., to arrive at an accurate estimate of cosOi, where Oi is the angle between the surface normal and the direction of incident radiation. A simpler method may be used for this purpose as described below. Real
surfaces
in outdoor
scenes
exhibit
a combination
diffuse component has been found to dominate reasonable to assume that the imaged surfaces
of diffuse
in commonly are Lambertian 65
and
occurring reflectors.
specular
refiectivities.
The
surfaces [21]. Hence, it is If L_ represents the gray
levelof
a pixel in the visual
to that pixel is related
image,
the relative
to the brightness
surface
orientation
of the surface
patch
corresponding
value by: L,, = Kp cosOi
+ Cv
(3)
where, Kp = p K_, p is the surface reflectance, K_, C,, are constants of the visual imaging system and are determined via calibration. The calibration process simply consists of imaging two different surfaces at known orientations to solar radiation and of known reflectivities, whence the constants Kv and Cv are easily
computed.
It is possible to obtain via stereoscopic image analysis, laser radar imagery, or from registered digital terrain data, the orientation of one elemental surface patch in the entire surface that is represented by a given image region. This orientation is best acquired for the elemental area that provides estimate, e.g., one that lies within a large planar patch. The region reflectivity p is then using equation
(3).
Knowing
p, the value of cosOi is easily
computed
at each pixel in that
a reliable computed
region
using
equation (3). The surface is assumed to be opaque, hence, the absorptivity is computed as a8 = 1 - p. The above procedure is applied to each region in the image to provide estimates of p and cosOi at each pixel
in the entire
image.
The assumption presence polished
that
viewed
of transparent objects surface). It is assumed
that
presented
4
Estimating
surfaces (e.g. that
are opaque
and are Lambertian
is sometimes
violated
by the
glass windows, lakes), or regions of specular reflection (e.g. a such regions in the imagery are detected by means other than
in this paper.
Surface
Heat
Fluxes
In this section, the various heat fluxes at the surface of the object are identified and the relationship between them is specified. A method for estimating these heat fluxes is then presented. This method uses values of surface temperature deduced from the thermal image, and surface reflectivity and relative orientation deduced from the visual image. Section 5 describes methods for interpreting imaged scenes using these
heat
Consider
an elemental
flow, the heat solar radiation, temperature denotes the
flux estimates. area on the surface
of the imaged
object.
Assuming
one-dimensional
heat
exchange at the surface of the object is represented by figure 3. Wi is the incident 0i is the angle between the direction of irradiation and the surface normal, the surface
is To, and W_b_ is that portion of the irradiation that is absorbed heat convected from the surface to the air which has temperature
by the surface. We. Tamb and velocity
V, heat
W,.,_d is the heat lost by the surface to the environment via radiation and Wcd denotes the conducted from the surface into the interior of the object. Irradiation at the object surface also from other scene components. As discussed in section 2, the magnitude of includes that emanating this absorbed irradiation is small when compared to total solar irradiation absorbed in visible and IR bands. The contribution of the former may therefore be ignored. At any given instant, applying the law of conservation of energy to the heat surface of the object and those flowing out from the surface, we have,
W.b,
= Wed + We, + W_ad
where,Wrod= 0.9 o (T: - T2mb), W_bo = Wi cosOi ao , 66
fluxes
flowing
into the
(4)
\1/
Wrad
V s Air
ov
Tamb
Figure
a denotes
the
convected
heat
3. Exchange
Stefan-Boltzman transfer
of heat
fluxes
constant,
is given
and
h is the
average
at the surface
_s denotes
convected
heat
=
h(T,
transfer
In order
image
to estimate
as discussed the
the solar
heat
magnitude of the incident radiation and the reflectivity of the imaged
in section
flux absorbed
-
object.
absorptivity
of the
surface.
T,,,_b)
coefficient,
surrounding air (e.g. velocity, viscosity, temperature, object's surface. We note that Wrad is immediately from the thermal
of the imaged
The
by Wcv
where,
;woo
(6) and
depends
on the
properties
of the
etc.), and on the geometry and the nature of the available when T_mb is known since T_ is deduced
2. by the
surface,
it is first neccesary
on a horizontal surface and then compensate surface. One approach is to directly measure
radiation using a pyrheliometer. Alternately, as was done in the appropriate analytical model may be used to estimate this quantity.
to determine
the
for the orientation the incident solar
experiments described later, an The variation (with day of the
year and time of day) of the intensity of solar radiation incident on a horizontal surface on the ground has been modelled by Thepchatri, et al. [22] based on the data presented by Strock and Koral [23]. The empirical model accounts for diurnal and seasonal variations. This model is used for specifying W_. Thus, knowing cos_ and c_ as described in section 3, Wab, may be computed using from equation (5). The convective heat flux is obtained by using equation (6). The temperature for the object's surface is obtained from the thermal image as described in the previous section. The ambient temperature Tamb is known. The problem therefore h. A plethora of empirical correlations hydrodynamic is fiat allows
lies in estimating the average convected heat transfer coefficient have been established for computing h for various thermal and
conditions [24]. The simplifying the use of convecion correlations
procedure for estimating the convected air temperature, the Reynolds number
assumption developed
that the portion of the surface being viewed for external flow over fiat plates [24]. The
heat flux is as follows: is computed, where the 57
knowing the characteristic
wind velocity and the length of the object is
Wabs
Figure
assumed
to be 1 meter.
4. Equivalent
The value of the
flow conditions exist. Accordingly, obtained and thence the convected the estimate
of convected
heat
thermal
circuit
Reynolds
of imaged
number
surface.
determines
the appropriate correlation is used. heat transfer coefficient h. Equation
whether
laminar
The Nusselt number is thus (6) is now used to provide
flux.
Having estimated the convected heat flux, the radiated heat flux, and the absorbed described above, the conduction heat flux is then deduced using equation (4).
5
Scene
irradiation
as
Interpretation
The estimated surface heat fluxes may be used to derive physically meaningful scene. Two different methods are discussed. The first approach assumes that of the
or mixed
scene is available,
and it consists
of the thermal
image,
the visual
interpretations only a single
image,
and
values
of the data set of scene
parameters obtained at a particular instant of time. The second method assumes that a sequence of data sets obtained at different time instants is available. The first approach is more suitable for scenes, the contents suitable containing
5.1
of which
for scenes
change
only vegetation,
Analysis
The estimated
frequently,
containing
objects buildings
of a Single surface
heat
e.g., one that that
automobiles.
over the sequence
The second of data
sets,
approach
is
e.g., scenes
and pavements.
Multisensory fluxes
contains
are stationary
may
be used
Data
Set
to evaluate
how well an object
can act
as a heat
source/sink. Thus a highly discriminatory feature may be extracted which is closely related to an intrinsic physical property of the imaged object. Considering a unit area on the surface of the imaged object,
the equivalent
thermal
circuit
for the surface
68
is shown
in figure
4. CT is the lumped
thermal
Object
Thermal Capacitance ( × 10 -6 Joules/Kelvin)
Asphalt Pavement Concrete Wall
1.95 2.03
Brick Wall
1.51
Wood(Oak) Granite
Wall
1.91 2.25
Automobile
Table1: capacitance
of the object
0.18
Normalized
values
of lumped
thermal
capacitance.
and is given by CT = DVc
where, given
D is the density
of the object,
by:
V is the volume,
and c is the specific
1 Roy = -_
heat.
The
resistances
are
1 and
Rr_d = 0.9a(T_
+ T2_mb)(Ts + T_mb)
From figure 4 it is clear that the conduction heat flux Wed estimated on the lumped thermal capacitance CT of the object. A relatively
in the previous section depends high value for CT implies that
the object is able to sink or source relatively large amounts of heat. An estimate of Wcd, therefore, provides us with a relative estimate of the thermal capacitance of the object, albeit a very approximate one. Table 1 lists values of CT of typical objects imaged in outdoor scenes. The values have been normalized Note
for unit that
automobiles
the and
volume thermal
hence
of the object. capacitance
for walls
Wed may be expected
and pavements to be higher
is significantly
for the
former
greater
regions.
than Plants
that
for
absorb
a
significant percentage of the incident solar radiation. The energy absorbed is used for photosynthesis and also for transpiration. Only a small amount of the absorbed radiation is convected into the air. Therefore, the estimate of the Wed will be almost as large (typically 95%) as that of the absorbed heat flux. Thus, Wed is useful in estimating the object's shown to be useful in discriminating between different the feature's the ratio
dependence
on differences
in absorbed
ability classes heat
to sink/source heat of objects. However,
flux, a normalized
feature
radiation, a feature in order to minimize was defined
to be
R = Wcd/Wobs Although imaged object.
the heat
flux ratio,
R
object, it is not discriminatory Other sources of information
=
Wcd/Wabs
,
does capture
a great
deal of information
5.2
results
Analysing
of using this approach
Temporal
If a temporal sequence conditions is available,
the
enough to unambiguously delineate the identity of the imaged are therefore warranted. Hence, information such as the surface
reflectivity, p, of the region which is derived from the visual image, and which is derived from the thermal image are also used to facilitate region experimental
about
Sequence
on real multisensory
of
Multisensor
average region temperature labeling. Section 6 presents
data.
Data
of multisensor data consisting of thermal imagery, visual imagery and scene then it is possible to extract a more reliable estimate of the imaged object's
69
Observe that the relationship heat radiation. capacitance CT of the object is given by:
relative ability to sink/source heat flux Wed and the thermal
between
the conducted
dTs Wcd= CT -d-i A finite
(backward)
difference
approximation
to this equation
Cr = w_ tl and t2 are the time instants
at which
CT as
(t2 - t,) (Ts(t2)
where,
may be used for estimating
(7)
- T,(t,))
the data
were acquired,
Ts(tl)
and T_(t2)
are the cor-
responding surface temperatures, and Wed is the conducted heat flux which is assumed to be constant during the time interval. However, Wcd does vary and an average value of (Wcd(tl) + W_a(t2))/2 is used in equation (7). Section
6 presents
to multisensory
6
experimental
results
obtained
by applying
the above
temporal
analysis
method
data.
Experimental
Results
The methods described in the previous sections outdoor scenes. Calibrated remote sensing data
were applied to real multisensory data acquired were not available along with values of ambient
from scene
parameters such as wind speed and temperature. Hence, thermal and visual imagery were acquired from a ground based imaging setup consisting of an Inframetrics infrared imaging system and a video imaging system. An anemometer was used to measure wind speed and a digital thermometer was used to calibrate the thermal imaging system so as to allow absolute temperature estimates as discussed in section 2. The two methods discussed in the previous section were applied to several sets of data which
were acquired
The results visual image 6 shows the
at different
obtained
times
of the day and during
using one data
set are presented
of a scene containing an automobile, thermal image of the same scene.
of this paper
were
used
to estimate
the
different
in figures
seasons
of the year.
5 through
8. Figure
5 shows
buildings, asphalt pavement and vegetation. The techniques described in the preceeding
surface
heat
fluxes,
whence
the
ratio
the
Figure sections
R = Wcd/Wab_
was
computed at each pixel. A histogram of these values was computed for each region and the mode of the histogram was found. This value was chosen as the representative value of R for the region. Figure 7 shows the values obtained for each region. As predicted by the discussion in section 5, automobiles produce
the lowest
vegetation
produces
value
of this feature,
the highest
pavements
and
buildings
produce
intermediate
In addition to the feature R, the average region temperature, and the surface used in a decision tree classifier to label regions as building, pavement, vegetation classifier used heuristic rules of the form: IF { R e [0.2, 0.9] AND p e [0.35, 1.0] } OR { R e [-.8, The resultant classification is shown in figure 8. The
method
of temporal
values
and
values.
analysis
hours. classes
Table 2 presents of scene objects.
the mean and The estimated
Except
for the concrete
and brick
of the scenes standard values
-.3]
} THEN
was tested
label
on data
reflectivity were also or automobile. The
= bldng
acquired
at intervals
of three
deviation of the value of CT estimated for different compare very favorably with those listed in table 1.
walls, the estimated
7O
values
for each class are of the same
order
of
ORIGINAL
PP_GE IS
OF POOR t_._ALITY
OR!GINAL BLACK
AND
WHITE
Figure
PP,GE' PHOTOGRAFH
5. Visual
image.
.57
Figure
7. Mode
Figure
6. Thermal
Figure
8. Region
image.
-,._
of feature
R.
71
classification.
Object
Average
(xl0 Automobile Concrete Brick
Wall
Wall
Asphalt
-_ J/K) 0.08
2: Values
of lumped
capacitance
-_ J/K) 0.08 0.37
0.37
0.38
1.05
0.46
1.5
2.7
Pavement
thermal
(xl0
Devn.
0.22
Vegetation Table
Std.
CT
estimated
using
the method
described
in section
5.2.
magnitude as listed in table 1, and are ordered in a similar manner. The walls do not compare favorably possibly due to the wide variation in wall thickness that is difficult to account for and also due to the unknown thermal conditions on the interior surface of the walls. In general, a significant offset may be expected in the estimated values due to the many approximations used in the computation heat flux estimates. Inspite of this limitation, it is obvious that the approach described above available a very useful and meaningful that the value of CT is a deterministic particular class of objects. by comparing the estimated interpretation interpretation
7
of the makes
method for the interpretation of multisensory data. Note also value which is completely defined by a physical definition for a
Hence, a deterministic measure of the technique's performance is available and true values of CT. Such a measure is not available in purely statistical
techniques. This is one of the major advantages of a phenomenological when compared to the purely statistical approach.
approach
to scene
Conclusions
A new method
has been described
for interpreting
scenes using multisensory
data.
The phenomenologi-
ca] approach combines information from the different imaging modalities to derive meaningful features. The approach is based on physical models of the energy exchange between the imaged surface and the environment. provide a measure
The thermal and visual images yield estimates of surface of the relative ability of the imaged surface to source/sink
pretation thus relies on a rough estimate of the lumped thermal capacitance been shown to vary widely for different classes of objects in outdoor scenes.
heat fluxes which in turn heat energy. The interof the object The developed
which has approach
was tested on real multisensory data. Due to the unavailability of a calibrated remote sensing data and accompanying values of ambient scene conditions, the testing was performed using terrain based imaging equipment. The approach described above may be easily applied to multisensory imagery acquired
by airborne
or satellite-based
sensors.
References [1] B.G. Lee, R.T. Chin and D.W. Martin, "Automated Rain-Rate Classification of Satellite Images Using Statistical Pattern Recognition", IEEE Trans. Geoscience and Remote Sensing, Vol. GE-23, No. 3, May 1985, pp. 315-324. [2] W.D. Rosenthal, B.J. Blanchard and A.J. Blanchard, "Visible/Infrared/Microwave Agriculture Classification, Biomass and Plant Height Algorithms", IEEE Trans. Geoscience and Remote Sensing, Vol. GE-23, No. 2, March 1985, pp. 84-90 [3] S. Di Zenzo, R. Bernstein, S.D. Degloria and H.G. Kolsky, "Gaussian Maximum Likelihood and Contextual Classification for Multicrop Classification", IEEE Trans. Geoscience and Remole Sensing, Vol. GE-25, No. 72
6, Nov.
1987,
pp. 805-814
[4] S.W. Wharton, "A Spectral Knowledge-Based Approach for Urban Land-Cover Discrimination", Trans. Geoscience and Remote Sensing, Vol. GE-25, No. 3, May 1987, pp. 272-282 [5] T. Lee, J.A. Richards, and P.H. Swain, "Probabilistic and Evidential Analysis", IEEE Trans. Geoscienee and Remote Sensing, Vol. GE-25, [6] D.G. Goodenough, Trans. Geoscience
Approaches No. 3, May
M. Goldberg, G. Plunkett and J. Zelek, "An Expert and Remote Sensing, Vol. GE-25, No. 3, May 1987,
[7] H. Asar, N. Nandhakumar and J.K. Aggarwal, Data", to appear in Pattern Recognition. [8] V.S. Whitehead, W.R. Johnson and J.A. Visible, Near-IR and Thermal-IR AVHRR GE-24, No. 1, Jan. 1986, pp. 107-112.
"Pyramid-Based
Boatright, "Vegetation Data", IEEE Trans.
Segmentation
Assessment Geoscience
[9] P.R. Christensen, "Martian Dust Mantling and Surface Compositions: Properties", Journal of Geophysical Research, Vol. 87, No. B12, 1982, [10] B.M Jakosky and P.R. Christensen, "Global Duricrust on Mars: of Geophysical Research, Vol. 91, No. B3, 1986, pp. 3547-3559. [11] N. Nandhakumar and J.K. terpretation", IEEE Trans. 469-481. [12] R. Siegel and J.R. 1981. [13] C. Ohman, 204- 212.
Howell,
"Practical
Aggarwal, on Pattern
Thermal
Methods
Radiation
[15] J.M. Jarem, J.H. Pierluissi and W.W. SPIE, Vol. 510, 1984, pp 94- 99.
[17] Horn
B.K.P.,
[18] Woodham
"Hill Shading
R.J.,
"Analysing
Thermal
Images
Multisensory
of Vol.
of Thermophysical
Sensing
Data",
Journal
2nd Ed.,
and
of Curved
Map",
Proc.
Surfaces",
Shape
from
Proc.
Empirical
the Reflectance
Reflectance
Mc-Graw
of SPIE,
Atmospheric
for Atmospheric
Map",
Applied
Artificial
Optics,
Vol. 313,
Occluding
1981,
Methane",
Vol.
Proc.
18, No.
of
1, 1979,
47.
Vol. 17, 1981, pp 117Boundaries",
pp
Data",
Vol. 19, No. 1, pp 14-
Intelligence, and
Co., New York,
Propagation
Model
of the IEEE,
Shading
ttill Book
140.
Artificial
In-
and R. Chellappa, "A Method for Enforcing Integrability in Shape from Shading Algorithms", on Pattern Analysis and Machine Intelligence, Vol. 10, No. 4, July 1988, pp. 439-451.
[21] J.M. Norman, Canopies and pp. 659-667.
J.M. Soils",
Welles and E.A. Walter, IEEE Trans. Geoscience
"Contrasts and Remote
Among Sensing,
Bidirectional Vol. GE-23,
[22] Thepchatri T., Johnson C.P., and Matloek H., "Prediction of Temperature by A Numerical Procedure Using Daily Weather Reports", Tech. Report Research, University of Texas at Austin. [23] Strock C., and Koral 2nd Ed., 1965. [24] Incropera 1981.
IEEE
Using a Combination and Remote Sensing,
of Remote
Measurements",
of Modelled
"Calculating
and the
Transfer,
Ng, "A Transmittance
[19] Ikeuchi K., and Horn B.K.P., "Numerical telligence, Vol. 17, 1981, pp 141 - 184. [20] R.T. Frankot IEEE Trans.
Heat
for Improving
R.W.,
Sensing",
Using
Interpretations pp. 9985-9998.
Analysis
Data
"Integrated Analysis of Thermal and Visual Images for Scene InAnalysis and Machine Intelligence, Vol. 10, No. 4, July 1988, pp.
[14] J.R. Schott and J.D. Biegel, "Comparison Proc. of SPIE, Vol. 430, 1983, pp 45 - 52.
[16] Horn B.K.P., and Sjoberg pp 17701779.
for Multisource 1987, pp. 283-293
System for Remote pp. 349-359
Image
IEEE
F.P.,
and
R. L., Handbook
De Witt
D.P.,
of Air
Conditioning,
Fundamentals
of Heat
73
Heating
Transfer,
and
John
Reflectance of Leaves, No. 5, September 1985,
and Stresses 23-1, 1977,
Ventilating,
Wiley
in Highway Bridges Center for Highway
Industrial
& Sons,
Inc.,
Press,
Inc.,
New York,
N91-15622 A Method Interval-Valued
for Classification Probabilities and H. Kim School
Laboratory
of
of Its
Multisource Application
P.H.
Swain
and Electrical and
Data using to HIRIS
Data
Engineering
for
Applications of Remote Sensing Purdue University West Lafayette, IN 47907, U.S.A. Tel: (317)494-0212, FAX: (317)494-0776 E-mail address:
[email protected] tent tion."
ABSTRACT
"evidential
informaresearch is framework can be in remote
sensing and geographic information systems. The methodology described in this paper has evolved from "evidential reasoning," where each data source is considered as providing a body of evidence with a certain degree of belief. The degrees of belief based on the body of evidence are represented by "interval-valued (IV) probabilities" rather than by conventional pointvalued probabilities so that uncertainty can be embedded in the measures. There are three fundamental problems in the multisource data analysis based on IV probabilities: (1) how to represent bodies of evidence by IV probabilities, (2) how to combine IV probabilities to give an overall assessment of the combined body of evidence, and (3) how to make decisions based on IV probabilities. The paper describes a formal method of representing statistical evidence by IV probabilities based on the Likelihood Principle. In order to integrate information obtained from individual data sources, the method presented in the paper uses Dempster's rule for combining multiple bodies of evidence. Although IV probabilities together with Dempster's rule provide an innovative means for the representation and combination of evidential information, they make the decision process rather complicated. We need more intelligent strategies for making decisions. This paper also focuses on the development of decision rules over IV probabilities.
1 INTRODUCTION The importance of utilizing multisource data in ground-cover classification lies in the fact that it is generally correct to assume that improvements in terms of classification accuracy can be achieved at the expense of additional independent features provided by separate sensors. However, it should be recognized that information and knowledge from most available data sources in the real world are neither certain nor such a body sometimes
as
The objective of the current to develop a mathematical within which various applications made with multisource data
A method of classifying multisource data in remote sensing is presented. The proposed method considers each data source as an information source providing a body of evidence, represents statistical evidence by interval-valued probabilities, and uses Dempster's rule to integrate information based on multiple data sources. The method is applied to the problems of ground-cover classification of multispectrai data combined with digital terrain data such as elevation, slope, and aspect. Then this method is applied to simulated 201 -band High Resolution Imaging Spectrometer (HIRIS) data by dividing the dimensionally huge data source into smaller and more manageable pieces based on the global statistical correlation information. It produces higher classification accuracy than the Maximum Likelihood (ML) classification method when the Hughes phenomenon is apparent.
complete. We refer to tain, incomplete, and
information
of uncerinconsis-
75
2 AXIOMATIC DEFINITION IV PROBABILITY
OF
when there is absolutely the probability of A. The basic probability
Interval-valued probabilities can be thought as a generalization of ordinary point-valued probabilities. The endpoints of IV probabilities are called the "upper probability" and the "lower probability." There have been various works intro-
fined in Shafer's evidence[6] has the the IV probabilities:
re(A)
satisfying I)
U : I] _ [0, I]
(2.2)
the
U(A)
following
_>C(A) _>0
for any Ae _
(2.4)
III)
U(A)
(2.5)
= 1 for any Ae[3
For any A, BeJ3 and < L(AuB)
R ax/i,_Ts
brightness
distribution
This completes one top-down shot. The two main stages are shown in Fig. 3.3 and Fig. 3.4 (the original image is Fig. 1.2). Fig. 3.3 shows the lowpass filter (in this case a 25x25 window lowpass was selected by VES) together with the local maxima. Fig. 3.4 shows the corresponding circles that survived the "radial brightness distribution" test. Each of these circles is assigned to a scene object
(tree).
Some
of the
trees
are
removed
If the interpretation process is started The parameter variation will produce
by the
final
test
by (START '(TREE)), two more lowpass filters
120
in METH0
(if standing
too
close).
the global rules will be applied. and this will result in new local
maxima, circles and trees. The search for contrary objects (in this test case a road was entered manually) leads to the elimination of trees that would grow in the middle of a road. The final result shown in Fig. 1.3 was obtained after two parameter variations (19x19and 3lx31 lowpasswindow).
Fig. 4 PROCESSING
THE
TEST
3.3
DATA
Local
maxima
Fig. 3.4
Circles
from
Fig.
3.3
SET
We took a small portion of each of the five images Fig. 1.5 a. - e. each showing approximately the same part of the scene. The size of these portions is 512x512 pixels (b. - e.) and 256x256 pixels (a.). All five images were processed with the standard VES tree-search (search for a default crown radius of 2,5m followed by two parameter variations (1,25m and 5m)). The original 512x512
Fig 4.1
5122 portion
of d.
Fig. 4.2
5122 portion
of c.
Fig.
Fig.
1282 portion
of d.
Fig. 4.5
1282 portion
of c.
Fig 4.6
4.4
121 ORIGINAL" BLACK
AND
WHITE
PAGE' PHOTOGRAPH
4.3
Circles
from
A correlation
ORIGINAL OF POOR
Fig.
4.2
result
PAGE
IS
QUALITY
images are shown for d. (Fig. 4.1) and c. (Fig. 4.2). Fig. 4.3 shows after the first top-down process. The final results (trees found) are portions of d. (Fig. 4.4) and c. (Fig. 4.5).
the circles found in Fig. 4.2 shown in detail for 128x128
The results of this experiment were very interesting: While even in the worst case (1:32000, a.) many of the large crowns were detected, there was no "perfect" interpretation in any five cases a. - e.. Of course, the best results were obtained for the larger scales (c. - e.). each result there were several trees missing that were found in another case. The same for erroneous artifacts, which don't show up in more than one result at the same location. conclusion - the desired result of the interpretation of the whole data set (a. - e.) would careful combination of the several results. And, working with "intelligent" vision systems, we favour a robust solution that doesn't require too precise and detailed instructions, similar ability
of a person
to identify
the
same
tree
in two different
image of the But in is true As a be a would to the
images.
As a first step towards this goal we tried the following procedure. We generated dot images of the five results. For each tree a dot mark located at the center of the circle representing the tree was produced. When two different results were overlayed and displayed in different colors, the resulting image was very similar to the dot patterns described by Glass [Gla69] and Stevens [Ste78]. In our case the patterns of one result may be converted to another one by assuming a superimposition of translation, rotation and a small change of scale. The remaining "noise" is caused by the individual height of each tree, and by the different position of the sun and viewing position for each image. In addition, due to the imperfect interpretation, some points are missing or added in the other image. Stevens called his patterns "Glass patterns" and he developed a loca/ algorithm for the correct correlation of associated points. We implemented Steven's algorithm and tested it on the dot images generated from the interpretation results of a. - e.. One result of a correlation between the two images shown in Fig. 4.4 and Fig. 4.5 is shown in Fig. 4.6. The results of this experiment were imperfect but very promising. Taken alone, Steven's algorithm is not effective enough for our patterns. This is due to the noise effects discussed above and due to the occurence of rather large point displacements. The algorithm will have to be adapted for our purposes - there are already several ideas for improvements. When viewed as one component of a larger vision system, even the actual performance of the algorithm is valuable. The correlation results will be processed by VES. Several heuristics may be applied, e.g. the fact that correlated trees should be of similar size. The correlation should also hold for more than two of the results (a. - e.). If there is a component in the system, that is able to determine species [Bis89,Pin90], then correlated trees must have the same species. Current research is addressing these topics.
5 CONCLUDING It has been
shown,
the tree at IVF
REMARKS that
the use
of multisource
data
can improve
the
quality
and
robustness
of the
interpretation result of a computer vision system. While synergic effects of this kind are well known, the proposed approach is also robust from another point of view. We do not need the geometric rectification of our multisource data to compare them. We also don't need complete or very accurate correlation results. The system is able of comparing two objects from two scenes just like a human interpreter looking at the two images. In a way the knowledge of a system like VES may be viewed as an alternate data source itself.
122
Many problems were discussedonly very briefly or not at all. The ideas about the representation of objects, processes and methods in VES are improved in the VS environment. This representation problem is closely coupled with the problem of control of the interpretation process. Methods like the one described above can help in getting a better assessment of the current interpretation result. Dealing with multisource data, the representation problem becomes even more difficult: While there is one individual object, there can be several scenes (several scene objects) and many images (many approach for a vision system in a natural in a man-made environment. reflected in fuzzy and robust
image objects). Furthermore we believe environment should be rather different
Fuzziness in shape models and methods.
and
morphology
of natural
that from
objects
a good the one
has
to be
ACKNOWLEDGEMENTS The author wishes to thank Renate Bartl and Horst in producing the experimental results presented Med.Kybernetik u.Al., Univ.Wien) for making their
Bischof for fruitful discussions and their help in this paper. We thank IMKAI (Inst.f. implementation of FRL available to us. This
research was funded by the following contracts: "Rechnerunterstfitzte interpretation" (Fonds zur F6rderung der wissenschaftlichen Forschung Jubil_iumsfonds d. Osterr. Nationalbank) und "Schwerpunkt Fernerkundung" Fonds zur F6rderung der wissenschaftlichen Forschung)
objektivierte Proj. Nr. (Projekt
Luftbild4489 und $38/2 des
REFERENCES [Bob88]
Bobrow X3J13,
D., 1988
et al.,
[Bis89]
Bischof, H. and Pinz, A., "The Use of Neural Networks for Species in Digital Images", in Pinz, A. (ed.): "Knowledge-based OCG Schriftenreihe 49, Oldenbourg 1989, (in German)
[Bur88]
Burt, P.J., "Attention 1988, pp.977-987
[Gla69]
Glass,
L., "Moir6
"Common
Lisp
Mechanisms
Effect
from
System
for Vision
Random
[Han78b]Hanson Scenes", Orlando,
A.R. and Riseman E.M., "VISIONS: A in Hanson, Riseman (eds.), "Computer 1978
[Hae87]
S., Tr_inkner
[Hav83]
H.
and
(eds.),
Nature,
A.R. and 1978
Aerial Photographs: Oberpfaffenhofen,
E.M.
Dots",
Eckstein
"Computer
W.,
The Path through 1987, (in German)
the
Havens W. and Macksworth A., "Representing Computer, Aug. 1983, pp.90-96
123
Specification",
in a Dynamic
[Han78a]Hanson Orlando,
Haenel
Riseman
Object
the
World",
Vol.223, Vision
Draft
Bottleneck",
Proc. 9.ICPR,
pp.578-580,
Systems",
Knowledge
Detection
to
Recognition of Tree Pattern Recognition",
Rome,
Aug.
Academic
Computer System Vision Systems",
"Automatic
submitted
1969 Press,
for Interpreting Academic Press,
of Tree
Crowns
in 2.DFVLR-Statusseminar,
of the
Visual
World",
IEEE
in
[Mar82]
Marr,
[Mat87]
Matsuyama, T., "Knowledge-Based Aerial Systems for Image Processing", IEEE Trans. 25, No.3, May 1987, pp.305-316
[Mat88]
Matsuyama, T., "Expert Systems for Image Processing of Image Analysis Processes -", Proc. 9.ICPR, Rome,
[Mat90]
Mates J., l__nsky P. and Yakimoff N., "Models for the Perception Random Dot Patterns", Biol. Cybern. 63, pp.71-80, Springer 1990
[Keo85]
McKeown D.M., Wilson A.H. and Imagery", IEEE Trans. on Pattern No.5, Sept. 1985, pp.570-585
[Min75]
Minsky, M., "A framework for representing Psychology of Computer Vision", Mc Graw
knowledge", Hill, 1975
[Nag80]
Nagao Plenum
Analysis
[Naz84]
Nazif IEEE 1984,
[Oht85]
Ohta Y., publishing,
[Pin88]
Pinz, A., "An Image-Understanding Infrared Aerial Photographs",
[Pin89]
Pinz, A., "Final Results of the Vision Expert System Based Pattern Recognition", OCG Schriftenreihe,
[Pin90]
Pinz A. and Bischof H., "Constructing Species of Trees in Aerial Photographs",
[Rob77]
Roberts, Goldstein, MIT, 1977
[Sch89]
Schneider, W., "Using Limits", FBVA-Berichte,
[Ste78]
Stevens, Spiringer
D.,
"VISION",
M. and Press,
Freeman,
Matsuyama New York,
A.M. and Levine Trans. on Pattern pp.555-577
1982
McDermott Analysis
T., "A Structural 1980
Image Understanding Systems and Expert Geoscience and Remote Sensing, Vol. GE-
- Knowledge-Based 1988, pp.125-133
'q'he
Interpretation
FRL
of Orientation
in Winston,
of Complex
of Outdoor
Natural
Aerial
The
FRL
Manual",
for the Atlantic MIT
of Locally
124
Parallel
Structure",
Biol.
"The
Photographs",
Color
Scenes",
VES", in Pinz, A. (ed.): Oldenbourg 1989
a Neural Network Proc. 10.ICPR,
(ed),
An Expert System", PAMI-6, No.5, Sept.
Pitman
in Color-
"Knowledge-
Interpretation City, IEEE
of the 1990
Memos
and
Remote Sensing for Forest-Inventory; Methods, Sonderheft, Wien, 1989, (in German)
K.A., "Computation 1978
P.H.
Expert System for the Recognition of Trees Ph.D. Thesis, TU Wien, Okt.1988, (in German)
Primer,
in
J., "Rule-Based Interpretation of Aerial and Machine Intelligence, Vol. PAMI-7,
M.D., "Low Level Image Segmentation: Analysis and Machine Intelligence, Vol.
"Knowledge-Based London, 1985
Composition
408
Possibilities
Cybern.
409,
and
29, pp.19-28,
N91-15626 Visualizing
Characteristics the
Shuttle
of
Imaging
David The
Johns
Ocean
Data
Radar-B
G.
Physics
Laurel,
Maryland
During
Tilley
Hopkins
Applied
Collected
Experiment
University Laboratory 20723-6099
Abstract
Topographic Contour
Radar
plotted
as
the
track
the
Fourier
SAR
P-3
same
are
spectra,
modulations, Visual
aircraft computed
compared
after
subtraction
yields
topography
perspectives
surface
tracks
fields
on
observed
distinctions considered
within
scattering.
The
the
Keywords:
Doppler
SAR in
space
of
Chile and
of
of
a
ocean
and
time,
in
October
waves,
image
of
wind of
insight
with
height
by
the
SCR. for wave
Threshold
of
as
of
generated SAR
of
rough
to
the
synthetic
processing,
wave
1984.
model
images
although
modulations
is
waves
(SAR)
made
for
(ROWS)
inversion
compared,
statistical
ocean
radar
modeling
are
rotating
Challenger.
Fourier
measurements data
endeavors
of
from
shuttle
aperture
texture
dynamic
these
imaging
radar,
ocean
are along
Spectrometer
space
and
Surface
variance
computed
spectra.
direct
the
experiment
height
Wave
the
noise
to
elevation
context
the
wave
spectral
and
coast
result
governing
SCR
surface the
mechanisms
of
were
synthetic
by
(SIR-B)
wave
Ocean
under
surface
somewhat
off
between
SIR-B
ROWS
observe
Radar
flown
similar
the
differing
it was
collected
Radar
spectra
the
from
to
to
wave
by
as
elevation
Imaging
plots
Ocean
acquired
NASA
surface
Shuttle
surface
aircraft.
spectra
ocean
sea
NASA's
dimensional
a
power
the
of
during
measurements
aboard of
three of
altimeter
measurements (SCR)
data
physical
aperture
computer
are
surface
radar.
graphics
Introduction
Remotely change
global
sensed in our
information
on
forthcoming
in
for
the
empirical
spatial height are
next
temporal slope
viewed
as
scale texture experiment.
The
from
along
and
NASA
Challenger
as
of
9 October
4
days,
spectra Walsh
have et
al.,
been
variety As
ground
surface
to
computed
1985]
and
12
from Radar
the
1984.
coast As
data
acquired
Ocean
Wave
125
a by
a
in wide
result, the
Spectrometer
Chile
ocean
the
Contour
[ROWS,
short(SIR-B)
space
(55°S,
of wave
sensors in
Radar
directional Surface
relation
remote
Imaging
be tool
range
correlations
of of
of
spaceborne
Shuttle
underflights
will
processes
measurements and
monitoring much more
a scientific
over
appreciate
during
southwestern
October
physical
radar
for and
atmospheres as
operating
to
state
and
emerging
airborne
conducted the
of
example, of
potential now exist
oceans is
sensors
track
sea
aircraft
approached
an
the sets
our
models
of
perspectives
long-scale
P-3 it
the
of
computer
a
offer data
Visualization
scales.
shaded
data Large
properties
decade.
theoretical data
and and
spectral
the
investigating
to
earth science environment.
shuttle
80°W)
on
each
surface
wave
Radar
[SCR,
Jackson
et
al.,
1985]
for
comparison
Aperture
Radar
[SAR,
characterized
by
lowest
sea
system
with
state a
a
fresh
occurred
with
field
was
observed
a
height
of
wave
about
set
on
is
of
imaging
SAP,
with
12
may
for
be
have
be
of
radar
been
SAR
[Tilley,
estimate using
image
present.
are
required
including sea
to
variety
of
states
and
coastal
authorities.
dynamics of
improve that The
is
power. remote over
are
A
of
object
126
the
ocean
that
be
time
of
the
for
dynamic is
restore
with
to
tilt
and
height
processing
ocean
wave
height
direction, ship SAR
a
response
wave
spectral of
on
Doppler
applied
surface
oceanographers,
research
restored
required
propagation
well track
based
of
SAR
not
along
partially
and
to in
estimates to
inverse
blurring
model
and
is
SAR
threshold
applied
Advances
interest of
can
power
sensor
Canada an
deterministically
the
stationary
wavelength
in
has
sensor
response
be
motion
theoretical then
remote
Montreal,
theory that
in
estimated
1987]
well
and
a broadband
noise.
image
may
surface
events
rough
later.
apparent
ocean
spectra,
distributions
the
is
based
facets
used
spectral
days
is
floor that can tilted toward
SIR-B be
SAR
derive
homogeneous
near can
modulation
model
empirically
Fourier
few
scattering it
a
Missisquoi
broadband
a
backscattering
[Monaldo, the
the
reduction
the
function
the
and
backscattering
for
wave
about
noise facets
upon
not
filters
domain
Speckle
of
are
approach
restored
learned
spectral surface angle
Baie
Chile
been
with
with
spectra
enhancement
spectral
response
over
of
random
has
imaged
groups
and
distribution
improve
by
SAR
from
modulation to
the to
signal
significance
variance,
surface
power
spectral
images
the
and
the
SAR
response
empirical of
applied
wave
techniques
the data track
of
wave of
domain.
hydrodynamic
limited
an
After
are
velocity
from
across
wave
restoration
23 ° incidence
However,
is
directional
in
image
surface a
distant
what
wavenumber
to
via
with
a
coast
rough
synthesis.
separate
track
apparently
This
and
storms
wave
shuttle an
by
a broadband of transient
collected
the
distribution
functions
this
again
track
when
developed
a significant
the
modulations
reduced
apply
the
stationary
operation off
waveheight
1987]
stochastic
SAR
This
response
[Tilley,
imaging
October
underflights.
individual
function
in
at
data
1984.
at
wavenumber
to
stationary
the
Non-homogeneous understood
1987]
down
spatially
obtained
to
to
developing
statistics
domain
transfer
looks
a
filtering
related
speckle
for determining random influence
7,
data
typical
transient
October
detected
along
estimate
normal
Fourier
elevation
1986]
Fourier
in
Hence,
it
to
October
II
waveheight
However,
methods as the as
[Tilley, on
the
induced
the
surface
Such
used
m
is
a well
12
The
driven
Doppler of
along
also
140
to
SAR
On
aircraft
modeling
set
measuring
propagate
the
wind
and
day
was
m.
propagating
data
diminished
radars
about
to
by
examined
modulation
surface.
m having
responds
applications.
better
empirical subtracted
the
the
in
4.6
northeast
This
following
to
to
non-homogeneous
the
as
m
Synthetic period
growing
the
SAR.
which
of
fields
characterized
developed
estimates
from the
The
transformed
significance. been
actively
northwest.
of in
1.7
380
so
day
it
wave
Fourier
well
ocean-imaging
on be
ocean
fast
might
turned
as
from
the
of
wavelength
SAR
varied
a consensus
from
last
day
influence
direction.
interest
oceanographic
height
and
four
texture.
necessarily and
in
occurred
m
from
The
an
of
backscatter
the
of
Homogeneous SAR
a
particular
and
m
October,
properties
velocity
state
270
computed
data.
appeared
reached
look
when
m
a wavelength
3.5
the
system
northeast
of
that
direction
state
sensors
with
80
spectra
image
October
sea of
power
height
about
sea
wavelength
90 ° from
i0
look
sloped
remote
swell
new
of the
highest
radar
wave on
modulations The
three
about
1986]
al.,
significant
steeply
technique.
wave
wave
et
-30 ° from
hydrodynamic
the
Fourier
Beal
wavelength
approximately of
a
with
is
for
captains to
develop
theoretical
descriptions
parameterizedby can
then
with
be
with
surface
topography,
(e.g., the statistics.
Synergy
of
Aircraft
The Chilean
SAR,
been radar
October
sensors
is
the
are
ROWS
have
data
field,
an
surface
inverse
by
grouping
Fourier
dimensional
On
at
these
12
October
a 380
direction, weaker
m
Both
of
when
only wave
at
modulations the
An
of
image
transform
of
applied
to
is
in
depicted
coverage
On carrying Both
i0 the
remote
I0 SAR
of
ROWS of
the and
spectral
m 2.
Once
of
SAR
the
the
scenes
surface
wave
of
the
topography
ocean
of
sites
are and
by
non-homogeneous
for The
Figure
2b 3
where
wave
SARwere sensors
at
the even
detected
SAR,
the
was
track
direction.
be
computed
tilt
ocean and long
ranging
its
velocity
400
m
wide,
inverse
to
as tilt
SARalso
Fourier function
modulations
of
along well
direction.
transfer
Figure similar
measurement
each
an
ib,
estimate
surface The
m wavelength
in A
as
flight
by
be
swell.
Figure to
via
imaging
380
in
SAR,
across
along
may
travelling
the
system
the
tracks,
also
wave
can
and
applied
that
represented elevation.
direct
shown
A
direction,
dominant
driven
a theoretical of
as are
shuttle
travelling
surface
the
la
flight
heading.
flight limit
for
surprising
wind
interaction
the
observed
space
in
ROWS
Figure
eastern
southerly
the
the
in
its
signal-to-noise
not
variance
aircraft
spacecraft
October
is
depicted along
more
functions
system
both
a
by
driven sea are of the surface
SCR
to
response
weak
after
spectra nearly
detected The
it
the
height
account field.
the
recreate
across
broadening
also
wave
spectrum
power
instrument's
the
occurring
wave
SAR
over as
the
so
swell
surface
low
spectrum.
backscatter
140 m wavelength wind generated visualization depicted
on this
estimates
similar
ROWS
propagating
are
detect
the
propagating
instrument
dominant
the
states
suppression
units
of
over
site, at
of
direction,
able
to
backscattered
near cause
variance
of
observed
to
visualizations
system,
systems
flight is
Chilean
spread
empirical
action
eastern
applied
measurements
sea
height
with
in
three
assessments
spectral
and
the
Therefore,
develop
have
systems
the
wave
SAR.
the
format
SAR
clutter
best
statistics
system,
the
wave
the
ROWS,
the
appears
or
these
is SCR
surface
m wavelength
detected
with
the
variance,
its
this
all
low
Comparisons
to
height
wave
general,
for
detection,
action
with
height
wavelength
apparently
confused
of
In
with
to
at
in
consensus
investigation signal
experiment
sites.
that 140
a
by
SAR
geophysical
ocean future
models.
misrepresented
the
compared
non-Doppler of
SIR-B
designing
wave
reach
transform
three
of
significance.
Comparison
the
sea
terms
measurements
be
spectra
and
using
directional
wind-driven
for
guide
wave
indicates
computer
in to
computing
computing
to
continuing
transformed
Intercomparisons
value
to
direct
can
Fourier
methodology
yield
m 4.
purpose
fresh
inverse
during
to
of
that
data.
Observations
the
able
considered
more
collected
units
height
elevation.
made
is
wave
make
Ocean
somewhat
of
served
SAR
for
applied
of
estimates
the
be
subject
or
processed
the
to
spectra, evaluate
that
modulations
statistical
to
data
were
algorithms
restoration
an
1987]
appeared
scene
the
common
although
various
is
in
potential
remote
encountered,
ROW been
section
Fourier
wave
SCR)
[Beal,
their
cross of
Spacecraft
all
spectra
assessing
and
and
have
reported
ocean
and
SCR
site
variance
ROWS
radar
analysis
compared
ocean
radars surface
of
empirical
swell
of
the
and
the
2a as a computer visualization is surface
topography
simulate
the
same
SAR.
Chilean more
site,
closely an
80
m
the
ROWS
aligned wavelength
127
aircraft along wind
and
the
space
shuttle
eastern
flight
directions.
driven
system
propagating
at
60 °
and
a
direction. longer
200
The
swell
m
for
both
respective
instrument
modulations
of
when
the
wavelength
spectral the
ROWS
cross
assumption of two-scale inverse transformed both function
statistics
of
elevation by
about
20 in
surface sea)
with
of
surface
plot
height
variance
Computing
and
The have
512
of
arrays
about
13
transfers
of
picture
minutes
using
disk
the
to
A
in
to
Comtal
i
DMA
was
also
unit x
can
i0"
be
The WAVE 2.2
of
for
using
Version a QUEN-16
and
to
80
correlation as
is
a
shaded
proportional
modulation.
in
the
in
Fourier
512 in
coordinate
data
computer
and
to
filtering
to to
the
over
transformed
to
prior
required
a PDPat
intensity
16-bit
been
Initial with
Corporation
developed
database
typically
have
workstations
facilities.
fast
was
and
accomplished
algorithm of
code
1984 graphics
32-bits be
partition
was
image of
the
system
was
512
x
apply inverse
restore
large
Fourier
wave
x
512
equipped
interfaced 8 bit
with
to
pixel
the
scenes
height
2 Mbytes
PDP-II/70 over
image
mm
R,G,B
roll
outputs
film
found
herein
system
which
now
surface
plots
developed
and
or
from
the
format
were
stands
color
from
i
alone
and
ocean Model
25
receiving
This
images
with
on
this
its
an
scenes 4007,
monitor.
to
photographed
in
a UNIBUS
memory
a pipeline delivering up to 30 color monitor. A Matrix camera, to
35
Figures
processor
was
interfaced
SCR
running
on
texture
from 1.0,
cm
scene.
expose
package
SAR
23 the
8"
image
inputs
from
tape.
PV-WAVE
visualized
x
display
SAR
software
The
Equipment
storage
program
controlling 512 x 24 bit
to
magnetic
(i.e.,
visualized
was
could
spectral
One/20
and
scaled
memory
hour
ocean
film. and
9-track
also
texture
(i.e.,
spectrum
computer
Digital
mass
Fortran
This
used
sheet
processing
word
i
SAR
second.
acquired
set
and
waves
collected and
(pixels)
optimized
transfers
LSI-II microprocessor a second to a 512
images
complex
Vision
allowing about
a
are
algorithms from
elements
About
significance
data
time.
action
surface spatially
wavelengths
departmental
filtering
Ocean
an
were
processing
purchased
64K
the
transformation.
This
The
SCR
height
bunching
different
Fourier
peripherals.
algorithms
to
differing
generated
wave
velocity
herein image
several
SAR decade.
between
magnetic
1981
using
system
the
and
presented in
the
minicomputer
beginning x
data
displayed
of
tilt
significance.
hours.
texture
the
spectrum was ocean imaging
compared
integration
and that
imaging
stationary
Technology
evolved
development 11/70
Displa7
and
assuming
wind
scene
elevation
4,
without
radar
processed that
surface
2
resonant
longer
the
height
surface
radar
by
to
about
and
the
their
velocity
ocean
image the
of
segments
compare
of
SAR)
km 2 ocean
and
SAR
of
for
tilt
SAR
are
flight
that
ergodic
Hence, the application wave
their
correction
describe the
images
by to
comparable
Figure
6
temporally
L-band
to
restore SAR
over
modulation
the
the in
3
opportunity
periods
properties to
for
to
after
violate the
from
dominated
surface
suffice
models. after
used
Figure
hydrodynamic
sensors
seas
130 ° sea
The
not
filtered
and
unique
waves
may
at
driven
remote
transient
Fourier in
wind
functions.
scattering before and
kilometers
a
acting m
two
the
SAR
section
traditionally
the
statistics
presents
and
and
propagating
of
response
radar
non-homogeneous
transfer
swell
amplitude
is
also
of
to
elevation
installed array
the
DECstation
information
a number
wavefront
a
in
on
processor.
figures
supported 3100 shade and a
by
128
computed
surface
rotation
desktop
offers plot
angle 3500
using
Visuals,
workstation a
VAXstation This
were
Precision
of
the ocean
interfaced
via is
being
PV-
Version
algorithms wave
perspectives.
processor
the
Inc.
height PV-WAVE,
a
Q-bus developed
to
jointly
by
Applied
Physics
that
a
512
about
20
and
Interstate x
SAR
new
on
x
32
bit
up
future
to
system.
x
8192
development
of
microwave
x
in
hydrodynamic
radars
64
bits
of
imaging
like
the
pixel Such
models
SCR,
SAR,
that
and
are
now
being
in
programmed
will
from
be
data,
SAR
could
a capability
will
shown
computes
computed
experimentation
scenes,
complex
have
transform
allowing
ocean
University
QUEN-16
perspectives
hours,
workstation.
Hopkins
the
Fourier
height
than Larger
this
Johns
with
algorithms
Wave
rather
algorithms.
8192
The
fast
filtering
in minutes,
improvements
and
experimentation
dimensional
spectral
filtering
producing
two
QUEN/VAX
data
Corporation
Initial
Basic
the
image
Fourier
with of
512
seconds.
tested
from
Electronic
Laboratory.
be
addressed
will
improve
with
processors
our
accelerate
understanding
ROWS.
Summary
Oceanographic of
NASA's
but
over
SAR
the
image
The SAR
to
October
needed
to
that
to
implement
a
quickly
remote
larger
sensors.
facilitate evaluation.
the
hurricane
of
of
data,
reduced
distribution
speed
and
networks, 1989]
are
Laboratory.
global
change at
assimilated
being Computer
in
at
visualization
129
advanced
is
simulations
emerging
time
will
in
their
and
computing University a
include
require
High
as
data
prediction
will
Hopkins
towards
science and
to
applied
assist
earth
in
or being
spaceborne
flight
models.
Johns
now
with
and
scales
and The
desktop
altimeter
environment
physical
workstations, developed
our
different into
a
directed
spills
the
workstation
imaging
for
is
prototyping
are
and
oil
contain
experiments
hypotheses
of
i0 SCR
developing
in
research
technology
may
rapid
3500
scanning
surveillance
collected
desktop now
with
theoretical
sensor
erosion,
a
filtering
visualization
on SAR,
modulation
is
as
ocean
of
theories.
VAXstation
of
SCR.
backscatter
imagery
algorithms
accelerate
graphics
of
a
1990]
comparisons
Monitoring
sensed
reviewed,
will
SAR
to
the
observed
visualization
Fourier
[Tilley,
remote
coastal
tracks.
remotely
Physics
fields
communication
Applications documentation
by
the
(generally
backscatter
serve
processing
of
study
Laboratory
to
purpose
hosted
model High
Physics
SAR
sea
modulation
1989]
interface.
simultaneous
tilt
Applied
unit user
ocean
and
general
of
obtained
surfaces
scale
driven
of
SIR-B
segment
information
synergistic
texture
those
that
short
wind the
theory
[Dolecek,
to
QUEN-16 driven
the
speckled
University
with
texture
Fourier
the
response
to
dimensional
part
texture.
variance
correlate
hydrodynamic
to
applied
as
Chile,
bunching
applied
a
with
the a
processor
a hydrodynamic
combined
[Jenkins,
that
of
similar
three
of
instrument
and
their
For
coast
environment.
menu
over
developing SAR
be
with
SAR
was
were
model
elevation
height
visually
height.
that
Hopkins
computing
transferred
to
velocity
array
can
personal
wave
and
Johns
shaded
southwest
supplement
wavefront
tool
the
also
The
as
resolution,
images
linear
spectra
plotted
spacecraft
comparable SAR
a
threshold
wave
and
at
spacecraft
surface
of
data
using
Fourier
were
noise)
indicates
information
The
were
long
off
data
data
speckle
The
power of
aircraft
function.
yield
estimate
plots
useful
QUEN
SAR
with 1984
ROWS
to
spectral
representation
their
as
size.
transfer
A
from surface
information
modulation
filtered
modulations
and
to
surface
yielded
different
parameterized
compare
referred
of
instrument. data
operated
have
topographic
and
were ROWS
visually The
obtain
response
functions by
regions
to
sensors
experiment
ocean
filtered system
remote
SIR-B
of that
space, speed
be data
technology Applied
combination
of
three-dimensional as
a
and
tool
empirical
microwave from be
graphic
scientific
data.
as
is
from
oceanographic
the
two-dimenslonal
to
surfaces
sensors.
physical
image
relationships
planned
rough
remote to
with
investigating It
scattering
insight
concepts
for
apply
that
The
these
can
be
result
processes
processing
between
of
resources
to
investigated this
governing
wind
models models
with
exemplary
the
methods
theoretical
of
radar
data
endeavor
generation
will
of
ocean
waves.
Acknowledgement Paul research Heeres work
Hazan
and have
has
Kenneth
for
advice
funded
Physics
Potocki
resources
contributed
been
Applied
and
identify
by
and
the
have
its
helped
define
development.
assistance
in
Independent
the
Quentin applying
Research
new
and
goals
Dolecek
of
and
this
Kenneth
technologies.
Development
This
Fund
of
the
Laboratory.
References
Beal,
R.
C.,
Jackson,
D.
Lyzenga
and
Spectra
with
F. W.
R.
Space",
L.
232,
"Spectrasat: Hopkins
Q.
E.,
Dig,, F.
Height,
Wind
Chile",
1985
No.
C.,
W.
Jenkins,
R. Dig.,
D.
No.
M.,
"A
Monaldo,
F.
SIR-B",
Johns
Tilley,
D.
Doppler
Imaging
G.,
D.
Techniques",
"Use
at
184-185,
APL
of
G.,
and
and
Moves
i,
Gonzalez,
Walsh,
Directional
F.
C.
D.
R.
Ocean
Wave
Ocean
Wave
Model
to Monitor
Ocean
Waves
from
Hopkins
APL
107-115,
1987.
Array
Processor",
Johns
C.
Peng,
Estimates
Y.
Remote
Into
"ROWS
for
SIR-B
Sensing
the
for
Ocean APL
for
Dig.,
Optical
Hopkins
J.
I.
Spectral
Global
Spectra
Methodology
Speckle
"SIR-B
Johns
SIR-B
E.
Symposium
Nineties",
of
Wave
Underflights
of
Digest,
Johns
Hopkins
2,
APL
1989.
Tech.
Radars",
No
Wave
APL
Practical
Hopkins
Hines,
Geoscience
I0,
3,
8,
Wavefront
Directional
"Computing
of and
F.
1989.
and
E.,
Irvine, Swift,
ROWS/SARApproach
APL
International
1985.
Tilley,
The
198-207,
E. N.
1986.
Dig.,
Glazier,
Speed,
804-811,
Spectra
A Hybrid
3,
R.
Comparison
Radar
Tech.
D.
Hines,
1531-1535,
APL
"QUEN:
i0,
Tilley,
E. "A
Scanning
C.,
G.
D.
Zambresky,
Johns
Jackson,
Tech.
F.
D.
III,
Science,
Dolecek, Tech.
Monaldo,
Aircraft
Prediction",
Beal,
M.
Hancock
8,
No.
Estimating i,
Determining
the
Engineering,
Wave
Enhancement Dig..
Tilley, D. G., "Anomalous Synthetic 1990 International Geoscience and
8,
No.
6,
with No.
Aperture Radar Remote Sensing
Spectra
from
the
1987.
Response
25,
Tech.
Wave
82-86,
Characteristics 772-779,
Fast-Fourier
i,
87-93,
of
1986.
Transform
1987.
Modulations for Symposium Digest,
Ocean Scenes", 2, 1083-1086,
1990.
Walsh,
E.
J.,
D.
W.
Hancock,
Measurements
in
Support
International
Geoscience
D. of and
E. SIR-B
Remote
Hines,
R.
Using Sensing
130
N. the
Swift,
and
Surface
Symposium
J.
F.
Scott,
Contour Digest,
2,
"Spectral
Radar",
1985
798-803,
1985.
1:::I r/l I1/
0
4.11-)
00J U
•IJ 0
U
0
:3 c_
0
r.-.I
,--40,1..I 0
0
,._
0
U
,,r..I
•1-1 ._
_
m
,--t
•I..10
_0 O0
r--t
k,I
.r-I
131
OR,G!,_'_,R.L _, ...,. OF POOff
QUALITY
_ }-I
(a)
1875
m
square
(b) 1200 square
Figure
2
SAR
three
dimensional
meter
(a)
swell
and
the
swaths
meters
wide
ment,
although
SCR
graphs
across
so
and
a
140 of
that at
(b)
meter the
sea,
remote
3 data a
surface
depicting
different
sets
elevation
wave
data
height
respectively, sensors.
The
approximate place
and
132
plotted for
propagating SCR the
time.
are
variance swath
contiguous
was
a
as 380
along
and
only
400
SAR
seg-
m
Figure depicted
3
A as
and
velocity
the
Fourier
compared tograms
200x200 a
bunching
segment
to
the
SCR
of
pixel
of
simulate topography intensity
the
Fourier
distribution
modulations
filter
with (d)
pixel
two-dimensional
of the
the
wave (c)
counts
of SAR height
along are
5
filtered the
wave
cross
SAR
section
separate
can
the
be
(b),
aircraft for
(a)
is
intensity.
distribution
computed
image
action
which tracks.
three
Tilt
included
data
in
can
be
Hissets.
133 ORIGINAL BLACK
AND
WHITE
PAGE PHOTOGRAPH
Figure 4 Long scale and short evident in a three-dimensional intensity that has been shaded from the unfiltered SAR image.
scale ocean wave correlations are surface plot of the SAR wave action with speckled data values derived
ORIGINAL 134
BLACK
AND
WHITE
PAGE PHOTOGIRAPH
N91-15627 A
PROPOSAL
TO THE
EXTEND OF GLOBAL
OUR
UNDERSTRNDING
ECONOMY
by Robbin Oakland Rochester,
R. Hough University Michigan
Manfred University Orono,
48063
Ehlers of Maine ME 04469
ABSTRACT To date, identified setting specific identified
global models have been just that. They have problems common to the peoples of the globe, without forth a basis for the specific actions carried out by peoples that could step toward a resolution of the problems. There is another way.
Satellites acquire information on a global and repetitive basis. They are thus ideal tools for use when global scale and analysis over time is required. Data from satellites comes in digital format which means that it is ideally suited for incorporation digital databases and that it can be evaluated using automated techniques.
in
The paper proposes the development of a global multi-source data set which integrates digital information regarding some 15000 major industrial sites worldwide with remotely sensed images of the sites. The resulting data set would provide the basis for a wide
variety
of
studies
The preliminary class of global helpful to local
results policy policy
central thesis be identified of
satellite
The
Problem
of and
this their
of
the
global
economy.
obtained to date give promise model which is far more detailed makers than its predecessors. proposal that utilization
major can be
industrial tracked
with
of
a new and It is the
sites the
can aid
images.
The focus of this paper is the role of policy, resources and the environment in economic and social development. The world view which it attempts to sketch for the reader will be alien to many who perceive economics as a policy science increasingly concerned with abstract "macro" entities. To be of use to humankind, policies for humans must be on a human scale. Moreover, it is of central importance that peoples be moved to perceive the objectives of the policies as important to them. To date, global models have been just that. They have identified problems common to the peoples of the globe, without setting forth a basis for the specific actions carried out by specific peoples that could step toward a resolution of the identified problems. There is
135
another way. Humans must have stories, images, habits of thumb to llve in complex environments and they Just have them as they relate to our world as a whole. Simply an atlas or even a world globe is an exercise in looking information than an individual can handle at once.
and rules don't browsing at more The
importance of manufacturing activity in the total market economy makes it imperative that manufacturing images and understandings be developed along with those which have to do with agricultural lands, forest lands, air quality, water quality, etc. The purpose of this proposal is to seek support for a project which will contribute to manufacturing images and understandings. Satellites acquire information on a global and repetitive basis. They are thus ideal tools for use when global scale and analysis over time is required. Data from satellites comes in digital format which means that it is ideally suited for incorporation in digital databases and that it can be evaluated using automated techniques. Background In order to approach the problems discussed above, a number of preliminary efforts have been undertaken. The first effort was a study of the relationship between economic activity in the 494 Rand-McNally basic trading areas and the sites of major manufacturing facilities. The 494 basic trading areas have 1361 sites of major economic activity. The 378 trading areas with manufacturing sites have a total employment in manufacturing of 20529027. The 116 trading areas without manufacturing sites have a total manufacturing employment of 1385727. The observation that 80 percent of the trading areas have 95 percent of the manufacturing employment indicates that an appropriate definition of "major" was utilized in the identification of the manufacturing sites. A simple linear regression of sites against manufacturing employment suggests that there are 12804.5 employees per site. The results are statistically significant at the one percent level. The scale of the coefficient (1/4 of the total reglonal mfg. employment) again points to an appropriate definition of "major". Moreover, it was possible by further work to account for nearly 85% of manufacturing employment on an industry by industry basis. The second effort undertaken was to construct a global database of regions which include as their centers, 738 cities chosen for their scale, their size in relation to their neighbors or their role as largest city in a nation bounded by geographic barriers or other regions. Based on the size given for the cities used as regional centers: Average Number
size of of cities
the largest per country
136
city
959173 3.67052
A profile of manufacturing employment for the regions centering on each city was computed based on the U.S. estimates. That is, each of approximately 13000 plant sites was assumed to provide the same level of employment provided by its counterpart in the United States. Assuming that a local labor-force is trained to work in manufacturing (L) and that fuel (F) and machines (K) are imported a production function would appear as: Output When estimates result is obtained for available: National R'2 F
= =
=
are 50
income
f(L,F,K)
aggregated countries
=
.45
by country the following on which World Bank data is
*
L'.54
*
F'.24
*
K'.I8
.912 158.915
In essence, over 90 percent of the variation in national appears to be accounted for by the site based employment estimates, fuel imports and machine imports. The close plausible magnitude of the coefficients are taken as preliminary evidence that the U.S. based estimates will reasonable employment A
third
substitutes for in the regions. effort
sought
to
the
actual
understand
levels
the
of
scale
of
the basis of the economic activity basis, commercial farms, trading facilities discussed above can
determine
of
scale
the
cities
supported
by
fit
and
serve
as
manufacturing
around the globe on sustain. On a global and the manufacturing the
income
a
cities which they facilities be shown to
given
region.
A fourth effort has been directed at the development of a multi-level hierarchical flat-file manipulation language which allows relational operations on digital geographic information systems as well as the storage of links to image collections. Language M is the result of that effort. It has been in commercial use for nearly two years. In a fifth project, DIRIGO - an image processing remote sensing data has been developed. The DIRIGO strictly to the Macintosh interface guidelines and users to become quickly familiar with the system. supports four file formats (i) image data, (2) ASCII of control classified intelligent
point coordinates or training images and (4) training areas interface insures that only
appropriate tasks. At
format present
can be DIRIGO
opened supports
for
area for files
system, for system adheres hence enables The system text files
statistics, classification. with the
(3)
the selected application (i) point operations such
An
as
linear and Gaussian contrast stretch and histogram equalization; (2) spatial filtering; (3) geometric correction such as image-tomap rectification and image-to-image registration using firstdegree polynomials and standard re-sampling techniques; and (4)
137
classification techniques such as parallelpiped, minimum distance, and maximum likelihood. Execution times for a 512 by 512 image with three bands range from seconds to approximately five minutes for a maximum likelihood classification with six classes. The results reported above give promise of a global policy model which is far more detailed local policy makers than its predecessors. It thesis of this proposal that major industrial identified and their utilization can be tracked satellite gives both are the
images.
rise simple already scale
The
to employment to grasp highly of the
concept and
that
a
major
new class of and helpful to is the central sites can be with the aid of
industrial
and income which cannot open to verification.
sensitive to plants studied
plant openings here. Indeed
facility
be ignored is Policy makers and closings these "local"
on
matters are matters of focus for legislatures, the press, trade unions, chambers of commerce and others. By global interdependence is meant that those actors must become aware of the kinds of changes occurring elsewhere on the globe that will influence the plants with which they are concerned. The paper industry in Green Bay should be vitally interested in changes in Finland. Objective
Project
The objective of the remotely sensed image
project being for each of
proposed the 13,000
sites worldwide. A latitude and longitude industrial classification can be identified this information and a scene which centers
is to major
produce a industrial
as well as an for each site. on the information
Given it
should be possible to identify the major site and a variety of the key facilities which are physically associated with it by interpretation. It would be expected that the working image so identified would be but a small fraction of the total image from which it would be extracted. That is, the industrial plant image would usually occupy less than one tenth of one percent of the total image. Thus each plant image would be expected to require only about 36k of storage. The complete global collection of images covering all sites of economic interest would be reduced to an easily manageable 1/2 gigabyte. A full working system for global analysis and modelling including detailed digital demographics for each of the regions and a variety of digital maps could be handled in less than 600 megabytes. Products
of
With the enabled. automated
images identified by site a variety of analyses In principle, interpretation could be supplemented analysis. A few of the many possibilities are:
.
A study specific
the
Project
of the requirements sites based on
of the
138
the industry analysis of
the
are by
images of the site. Buildings, parking lots, water sources, retention basins, storage space, special facilities, etc would be open to examination. A comparison characteristics
.
of
image features of the plants
to known from other
sources.
Such analysis would, for example, make it possible to distinguish integrated manufacturing facilities from assembly plants, consider power requirements and siting, the relationship to common public facilities, residential spaces, transport networks and the like. A
.
third
form
of
analysis
tracking of these of the characteristics known economic and plants. The most effort is
.
would
proceed
with
the
sites
over time and the relating of the tracked images to the operating characteristics of the
straightforward a digitized
product industrial
of the proposed atlas of the world.
The resulting product would have an exceedingly wide range of potential uses. It is possible to compare potential industry sites based on the characteristic parameters of other existing industrial sites. If criteria non-image be possible
.
can be established information of the to rate potential
information. principals
Earlier includes
associative evaluations.
retrieval
It would current) information
work the
combining image global database, sites based on
in this development
systems
area
for
use
by the linear in
and it will this project
comparative
be possible to include other (future and satellite images with other spectral (e.g., thermal, mid-infrared, microwave
etc.) and tie this together with SPOT's high spatial resolution. This would allow multispectral, multitemporal, and multispatial site assessments. References
Ehlers, Advanced
Manfred. Imaging,
Folland, Relationship
Sherman T. Between
Agricultural Hough,
1990, May,
Robbin
Land, R.
Manipulation of systems Research,
Their 1990,
Mac-Based 65-67.
and Hough, Robbin R. Nuclear Power Plants Land
and
Own pp.
Economics,
Hough,
Tor
Remote
Some and
forthcoming H.,
Hierarchic Relations, Baden-Baden, 1990.
139
Database Advances
Sensing
System,
Evidence the Value
of of
February Tools in
for
1991. the
Support
a
Hough, Robbin R., Natural Language and Geographic Information Systems, Proceedings of a NCGIA Workshop on Geographic Information Systems, University of Maine, 1990. . Specialization in Systems Research University of Windsor
and
and the Ecology of Microcomputers, Cybernetics, ed. George E. Lasker, and Oakland University, 1989.
• Evolutionary Process on Adaptation: Environment Calhoun, New York: Frederick
in
Hierarchical and Population, Praeger, 1986.
140
Systems, ed.
Advances
Perspectives John C.
SUMMARIES
141
143
PRL_EDiNG
PAGF" BLA_K
NOT FILMED
r,_
0000
_
_
O0
__
_
v V
_
°
_
¢)
I:_
E
R
_
r_
°
""
VV
e" 0
144
Summary
of Types of Data Fusion Methods in Workshop Papers
Sylvia Lockheed
S. Shen
Palo Alto Research 0/96-30,
3251
Hanover E-Mail:
Lab.
B/251
St., Palo Alto,
Phone:
Utilized
(415)
CA
94304
354-5019
[email protected]
ABSTRACT This paper
gives
a brief
integration
methods,
also gives
a summary
gration
in Remote
utilization
overview
namely
the recent
imaging
ent portions olutions,
fumishing
geophysical, these
payloads of a broad
sampling.
in their
Data
fusion
level
fusion
data sources pixel.
In this case,
form Sensory
registering rotational
registration
from
the images, shifts,
are pixel,
sensor
produce
at different
Data
Inte-
detailing
the
data
platforms covering
spectral
information
studies.
of analog
data
geometric
sophisticated
multisource
differoceanic,
In addition These
properties, data,
res-
such as aerial
for researchers.
characteristics,
that
and spatial
for terrestrial,
and planetary
conversion
data
into three
sensor
sources.
reference These
according
and
advanced
of multiple
of data
to pho-
data
are
temporal analytical
images
for relative and intensity
of a scene
145
translational distortions
at which
techniques.
resolution
performed obtained
common
to all
shifts,
pix-
for each
at the pixel-level. from different
It is accomplished magnitude
of each image.
fu-
Pixel-
for each of the 'new' are then accumulated
fusion
time are formed.
to the stage fusion
spatial
measurements
measurements
example
at different
correcting
as well as geometrical
types
and decision-level
with a pre-selected
ground
is a typically
namely
of different
are also available
feature,
pixels
and/or
comparison
the same
and
must be developed.
'new'
from the original pixel-by-pixel
sors or taken
types
involved. Image
increasingly
paper
TECHNIQUES
sensors
of useful
data, digital
can be categorized
The three
These
surveillance, data
used
of data
The
on Multisource
methods
FUSION
spectrum
amount
radiometric
these
techniques
els are derived 'new'
sensory
techniques
techniques
place.
tremendously.
enormous
format,
data fusion
sion takes
the number
technology,
and geophysical
To fully exploit
or numerical
in sensor
reconnaissance,
and airborne
topographical
heterogeneous
DATA
with
types
applications.
of the electromagnetic
meteorological,
spacebome
tographs,
users
science
Three
are discussed.
Workshop
fusion
OF MULTISOURCE
has increased range
techniques. fusion
at the IAPR
the type of data
data sets in earth
advances
data fusion
and decision-level
presented
categorizing
1. OVERVIEW
carry
feature,
of all the papers Sensing,
of multisource
With
of multisource
pixel,
sen-
by spatially differences,
Pixel-level
fusion
allows different sensoryor ground reference Feature-level
fusion
techniques
generally
information
be accumulated
start with applying
image
for each
analysis
'new'
techniques
pixel.
to extract
some features from each data source independently. Certain measurements of the extracted tures are derived from each data source and these feature measurements are then integrated. instance,
when
both visible
and thermal
infrared
mogeneous intensity can be extracted value and average surface temperature mal infrared gion-level various
images
respectively.
in this example. versions
For example,
data
are available,
regions
of nearly
using image segmentation techniques. Average of each region can be calculated from the visible
The intensity
Decision-level
of interpretation
interpretation.
image
and temperature
information
or interpretation-level
obtained
fusion
from the different
in the case of image
ho-
intensity and ther-
are fused
at the re-
deals with integrating
data sources
classification,
feaFor
to arrive
the
at a consensus
the interpretation
or classification
results can be represented in terms of probability assignments. Bayes rule and Dempster-Shafer's rule of combination are often used as a means to reinforce common interpretation and to resolve differences amples
in order
to arrive
of decision-level
A summary Remote
at a more
fusion
of all the papers
Sensing
is presented
complete
given
at the IAPR
in the next section.
each paper are discussed. Fusion techniques level fusion. The utilization of multisource also briefly
and accurate
The paper Robinson
entitled
and Tilton
"Refinement discusses
data through
the use of satellite
TM images,
finds the edges
data
to mask
ence
data
Workshop
out those
edge
the ground
OF WORKSHOP
of Ground
Reference
to refining
image
More
from
data.
This system ing process,
Integration
in
Data
and data fusion
methods
used in
edge
points
"Near Ground
describes
detail
the approach
and uses the edges
that are beyond
is categorized
level
Data"
segments distance
by
reference the Landsat
from the ground
a certain
as a feature
Image
to the ground
reference
from the refer-
integration
method
where
data and Landsat TM image data are fused. and detailed edge information be added to
Level
a workstation
Sensing
between level image
changes
"Integration
an approach
used to process
biomass.
detected
of SAR to fusing
near ground
No multisource
and DEM information
software
level image
data fusion
from Landsat
data will be studied
processing
of Vegetation" system
by Rasure, clusterlabeling
has been
image
analysis
consists of a low level segmentation process, a supervised and unsupervised an object feature extraction process, a classification process, and a region non-living
based
for Spatial
Chorus.
near ground paper
with Segmented
called
The system from
Data
and adding
data.
er, correlation
describes
ex-
PAPERS
specifically,
the segmentation,
This approach
entitled
and Gage
The
on Multisource
The data types
an approach
segmented
points.
reference
The paper
biomass
are typical
are categorized into either pixel, feature, or decisiondata sets in earth science applications by each paper is
the edge information extracted from ground reference This fusion allows reference edge error be corrected
process.
They
described.
2. SUMMARY
Sauer
interpretation.
techniques.
data
is discussed
TM image
data
to distinguish
in this paper. and those
living Howev-
observed
from
in the future. Data from
146
-- Geometrical SAR
images
Considerations" and
Digital
by Kropatsch Elevation
Model
(DEM) databasedon establishingsomegeometricalrelationsbetweenthedatasets.Layoverand shadowregionsaredetectedin SAR images. Suchregionsarealsofound independentlyusing DEM data. Informationfrom bothdatasetsarethenaccumulatedthroughgeometricalmatching of theselayoverandshadowregions. This fusiontechniqueis consideredto beatthe featurelevel wherethefeaturesarethe layoverandshadowregions. The paper entitled "TowardsOperationalMultisensorData Registration"by Rignot, Kwok andCurlanderaddressesthe problemof automated precision registration of multisource image data acquired
from a number
presented. data
The first technique
such as Landsat
tered. then
The
spatial
selection
us to accumulate
resolution
way Spruce
Forest
sensing
or damage
in forested
ples collected TIMS,
The paper ing Infrared on integrated the visible image
Discrete
intervals
face and the environment face temperature level.
When
performed
allow
information
the information at the feature
and surface temperature values based classification scheme. The
paper
Probabilities fying
entitled
and Its Application
multisource
probability
"A Method
which
data in remote is a generalization
Both
at a pre-seconsidered
to
MSS
is performed Data
into distinct
for each region
for Classification
of the point-valued
147
defines
: Analyz-
the imaged
pixel.
Here,
image
what
probability
Data
discusses is called designed
the sur-
data fusion
Aggregated
Using
IR sur-
at the pixel
and used as discriminants
by Kim and Swain
The authors
level.
The thermal
between
class categories,
of Multisource
NS001
approach based In his approach,
intensity.
regions.
sam-
to facil-
and TM,
Integration
from the visible
are the segmented
content, from
at the pixel
heat flux for each values
stress
and nitrogen are obtained
of energy
Nor-
of using
sets are resampled
homogeneous
the exchange
regions
Data"
the problem
as Landsat
to Multisource
of surface
the features
data
of Stressed
describes a region classification data of remotely sensed scenes.
with the intensity
sensing.
such
of nearly
describing
to HIRIS
discrete
data
Approach
are computed
and tech-
and differentiate
measurements
the data fusion
is used to classify
level where
These
sensed
the estimation
is fused
discusses
chlorophyll-a
into regions
model
pixel
Measurements
sets such as foliar
Therefore,
is first segmented
and Ground
and fluorescence
and Visible Data" by Nandhakumar analysis of thermal IR and visible image
images
matching
is, in general,
to monitor
"A phenomenological
are regis-
estimation.
for each
Registration
the sensory data
feature
parameter
sensors
by Banninger
over the test sites.
and a phenomenological
the different
This
measurements
with remotely
and FLS/PMI.
entitled
data
reflectance
integration
AIS-2
Assessment"
data, and ground
areas.
from
are
level.
Reflectance,
Damage
and foliage
at 50-m
information
TMS,
for Forest
to simulate of optical
for transformation
involved.
at the pixel
techniques
types
images.
from different
to all sensors
(DEM)
such as edges
the different
of tie points
Fluorescence,
data, laboratory
leaf area indices, itate
common
Model
of registration
the various
features
between
Two types
Elevation
therefore
information
of data fusion
"Combined
sensors.
the Digital
first extracts
the manual
example
The paper remote
technique
remote
and SPOT,
features
allow
be a typical
uses
Seasat
the extracted
replaces
techniques lected
TM,
second
matches
nique
of different
is
intensity in a rule-
Interval-Valued
a method
of classi-
the interval-valued to represent
the pos-
sibility of smalldeviationsfrom the unknowntrue probability. Their approachtreatseachdata sourceasa bodyof evidence,representstheevidenceprovidedby eachdatasourcein termsof interval-valuedprobabilities,andusesthe Dempster-Shafer'srule of combinationto integratethe interval-valuedprobabilitiesform differentdatasources.This integrationis thereforecategorized as to be at the decisionor interpretationlevel. This methodcan combineparametricas well as nonparametricinformation. The paper"ImprovedDisparity Map Analysis Throughthe Fusionof MonocularImageSegmentation"by Perlantand McKeown first addressesthe issueof using the segmentationof the monocularimagery to improve the estimatesof three-dimensionalscenestructure,namely the scenedisparity map. Their approachgeneratesthe initial disparitymapfrom a stereopair of imagesusing area-basedand/orfeature-basedmatchingtechniques.Then the surfaceillumination information providedby a monocularimageis usedto segmentthe imageinto regionsof nearly homogeneous intensity. Basedonthe assumptionthatsuchregionscorrespondcloselyto physical surfacesin the scene,the region informationis usedto removemismatches.Here,the disparity informationextractedfrom stereopairis fusedwith segmentation resultsobtainedform monocular imageatthe featurelevel wherethe featuresarethesegmentedregions. The authorslater address the problem of using a number of different region segmentationmethodsand stereo matchingtechniquesto improve building extractionaccuracy.Eachpair of region segmentation andstereomatchingtechniquesproducesa versionof building extractioninterpretation.The variousversionsof interpretationarethenusedin a votingprocessto arriveat a consensusinterpretation. The information integrationusedhereto achievea more completeandaccuratebuilding extractionis consideredto beat the decisionor interpretationlevel. The paperentitled "Useof InformationFusionto ImprovetheDetectionof Man-MadeStructure in Aerial Imagery" by ShufeltandMcKeown addresses the problemof building information fusionin aerialimagery. Sinceit is assumedthatno singledetectionmethodwill accuratelydelineatebuildings in every scene,a cooperativemethodis proposed. Variousbuilding extraction techniquessuchastheonesbasedon edgeanalysis,shadowanalysis,andstereoanalysisareused to producebuilding delineations.Thedifferentdelineationresultsaresuperimposedto generatea moreaccuratebuilding interpretation.Quantitativemeasuressuchasbuilding percentage,backgroundpercentageand branchfactor are utilized as a meansto evaluatebuilding extractionresuits. In this study,only onetype of sensorydata,namely,the aerial imageis used. Therefore, fusionis not performedusing differentsensorydata,but ratherusingthe differentdelineationresuitson the sameimagedata. The informationfusedis the edgeinformation. It is thereforecategorizedas a featurelevel integrationmethod. The paper"A ComputerVision Systemfor the Recognitionof Treesin Aerial Photographs" by Pinz describesthe conceptof a computervision systemcapableof finding treesin infrared aerialphotographs.Genericdescriptionof a type of anobjectis integratedwith the imageobject wherean objectis, in this case,a tree. The treerecognitionresultsfrom aerialphotographstaken atdifferentresolutionscalesandundervariousconditionsarealsointegratedatthe feature,namely tree,level.
148
The paper "Visualizing Characteristicsof OceanData CollectedDuring the ShuttleImaging Radar-BExperiment"by Tilley discussesthe computationof oceanwavespectra(powerspectra of the Fouriertransform)from SIR-B SurfaceContourRadar(SCR)dataandthe comparisonof theseclustersof energywith thosecomputedfrom theRadarOceanWaveSpectrometer(ROWS) dataandthe SIR-B SyntheticApertureRadar(SAR) datato parametrizemodelsof oceanimaging. No datafusionof thesethreetypesof sensorydatais usedin this study.Fusionwill, however,beconsideredin the future. The paper"A proposalto ExtendOur Understandingof the Global Economy"by Hough and Ehlersproposesthe developmentof a global multisourcedata setwhich integratesdigital information including remotely sensedimagesregarding 15000major industrial sitesworldwide to tracktheir utilization asa basisfor a varietyof globaleconomicstudies. No specificdatatypesor fusiontechniquesarementionedin this conceptualpaper.
149
Summary of Types of Data Output Produced by Studies Described in Workshop Papers Axel J. Pinz Institute
of Surveying and Remote University of Agriculture Peter Jordan Str. 82 A-1190 Wien, Austria Phone: (43-222) 342500-546
Sensing
There were a total of 12 presentations at the IAPR TC7 Workshop. Most of them dealt with the description of systems. While the two previous summaries discussed the input and processing aspects of these systems, this summary discussed the output aspect. Many contributions were concerned with an improvement or a kind of refinement of results by use of multisource data. The improvements are either in overall accuracy or in robustness. The output may be categorized as either a better segmentation, an improved symbolic description of the scene, or a more robust classification. These "improvement-papers" are: • Jon Robinson:
The output is a refined data set of edges into a refined ground cover label map).
• Tom Sauer:
The analysis process deals with classification, region analysis and spatial information. In its current state of development the system is separating vegetation from background. The final output is the percentage of ground coverage by specific vegetation classes
* N. Nandakumar:
In this combination of thermal and visual information, the thermal capacity is calculated and used to improve a segmentation, and to label various classes like pavement, vegetation, car, etc.
• H. Kim
and
P. H. Swain
(which
(presented by J. C. Tilton): The integration DEM data leads to a more robust classification.
can
be translated
of multispectral
and
• Frederick Perlant: • Jeffrey Shufelt:
These two papers from David McKeown's group at CarnegieMellon University discuss information fusion. There are several different processes run on the same image or on different images (stereo pair). The output of these processes in than fused yielding an improved result. In Peflant's work the output is a segmentation. Shufelt ends up with a set of boundaries delineating the objects of interest (e. g. houses).
• Axel
Having several images of the same scene, the first step of .process!ng leads to several symbolic description of this scene. The integration (fusion) of theses results yields an improved and more robust symbolic description of the scene objects (in this case, trees).
Pinz:
151
PRECEDING
PAGE
E:LAI"_K NO] ...... I_L..M._"*
The following contributions cannot be categorized so easily (as "improvement-papers"). seems that the desired output of these systems wouldn't be possible without multisource integration: Walter
Kropatsch:
It data
The integration of SAR, DEM and knowledge results in a geocoded SAR image. Furthermore, Dr. Kropatsch can map additional information (e.g., slope) into the original SAR image, providing means for a better interpretation of the original image.
• Eric Rignot:
This is going to be a very of registered and resampled
• C. Banninger:
The integration of a few Landsat pixels with a very detailed ground data set is used for an optimal positioning of the pixel grid. The outputs of this process are correlation results and models.
• David
Since the original radar image of the ocean appear very uniform to an human interpreter, the first task to solve is the proper visualization of the data. Furthermore, Dr. Tllley hopes to gain more insight into imaging mechanisms of SAR, and to uncover information in the speckles.
• Robbin
Tilley:
Hough:
huge system. The output data at uniform scale.
will be a pack
A database systems of this kind would be able of producing manyfold outputs depending on the query. It could be used as a tool for economic forecasting, planning and analysis.
152
APPENDIX Workshop
Participants
153
PARTICIPANTS Richard
Arens
Walter G. Kropatsch Institute for Technical
GTE Government Systems 1700 Research Blvd Rockville, MD 20850 Tel: (301) 294-8430 Cliff Banninger Institute for Image Proc. Graphics Joanneum Research
& Computer
Robert Losa USDA/NASS Rm 4168 - South Bldg Washington, D. C. 20250 Tel: (202) 447-9295
Wastiangasse 6, 1-8010 Graz, AUSTRIA Tel: 011-43-316-8021-0 Fax: 011-43-316-8021-20 E-Mail: banninger%rzj, cunyvm.cuny.edu
fgi-graz.ada.at@ David
Applied Research Corp. 8201 Corporate Drive Landover, MD 20706 Tel: (301) 805-0379 or (301)
M. McKeown
Digital Mapping Laboratroy School of Computer Science Carnegie Mellon University Pittsburgh, PA 15213 U.S.A.
David W. Case
459-8442
Tel: (412) 268-2626 E-Mail:
[email protected]
Long S. Chiu General Sciences Corporation 6100 Chevy Chase Drive Laurel, MD 20707 Tel: (301) 953-2700
N. Nandhakumar Dept. of Electrical Engineering Thornton Hall, Rm E-210 University of Virginia Charlottesville, VA 22903-2242 Tel: (804) 924-6108 Fax: (804) 924-8818 E-Mail:
[email protected]
Edward A. Dunlop Center for Remote Sensing College of Marine Studies University of Delaware Newark, DE 19716 Tel: (215) 430-6549 E-Mail: dunlop@ freezer.it.udel.edu Marcus
Informatics
Technical University of Vienna Treitlstr. 3 A. 1040 Vienna, AUSTRIA Tel: 0I 1-43-222-58801-818I Fax: 011-43-222-569149 E-Mail:
[email protected]
Mishh
Pavel
Bldg 420 Stanford University Stanford, CA 94305 Tel: (415) 725-2430
[email protected]
E. GIenn
MITRE Corp. 7525 Coleshire Dr. McLean, VA 22102 Tel: (703) 883-5386 E-Mail:
[email protected]
Frederic
P. Pedant
Digital Mapping Laboratory School of Computer Science Carnegie Mellon University Pittsburgh, PA 15213-3890 Tel: (412) 268-7552 E-Mail:
[email protected]
Dr. Robbin R. Hough Oakland University Rochester, MI 48063 Tel: (313) 651-0820 Fax: (313) 651-4071 E-Mail:
[email protected]
155
PRECEDING
PAGE Bt.A['_K
NOT
FILMED
Axel
J. Pinz
Inst. of Geodesy and Remote Univ. of Agriculture Peter Jordan Str. 82 A- 1190 Wien, AUSTRIA Tel: (43-222) 342500-546
Sylvia Shen Lockheed Palo Alto Research 0/96-30, B/251 3251 Hanover Street Palo Alto, CA 94304 Tel: (415) 354-5019 E-Mail:
[email protected]
Sensing
Eric Rignot Jet Propulsion Laboratory 4800 Oak Grove Drive
Lab.
Jeffrey Shufelt Digital Mapping Laboratory School of Computer Science Carnegie Mellon University Pittsburgh, PA 15213 Tel: (412) 268-3884 E-Mail:
[email protected]
California Institute of Technology Pasadena, CA 91109 Tel: (818) 354-1640 telex: 675-429 Fax: (818) 354-3437 E-Mail:
[email protected]
Stan Stopyra GTE Government Systems 1700 Research Blvd Rockville, MD 20850 Tel: (301) 294-8430
Jon Robinson ST Systems Corporation 4400 Forbes Boulevard Lanham, MD 20706 U.S.A. Tel: (301) 794-5200 E-Mail:
[email protected]
David G. Tilley The Johns Hopkins University Applied Physics Laboratory MS 23-346 Johns Hopkins Road Laurel, MD 20723-6099 Tel: (301) 953-5000 x8644 Fax: (301) 953-1093 Telex: 511303
Tom Sauer University of New Mexico Dept. of Electrical and Computer Engineering Albuquerque, NM 87131 Tel: (505) 277-6563 Fax: (505) 277-1439 E-Mail: sauer@ bullwinkle.unm.edu
E-Mail:
davet@
fermi.apljhu.edu
James C. Tilton Mail Code 936 NASA GSFC Greenbelt, MD 20771 Tel: (301) 286-9510 E-Mail:
[email protected] [email protected]
Andrew Segal University of Illinois Dept. of EE CS M/C 154, Box 4348 Chicago, IL 60680 U.S.A. Tel: (312) 996-5486 E-Mail:
[email protected]
E. D. Zeisler 8242 West Buckspark Potomac, MD 20854 Tel: (703) 883-5768
Robert Series RSRE St. Andrews Road, Malvem Worcs WR14 3PS UNITED KINGDOM Tel: (+44) 684-5784 E-Mail:
[email protected]
156
Lane
or
Report
Nalona_/_onaut¢sand _oaceAdcr_r_lralOn 1. Report
Documentation
2. Government
No.
Accession
Page
No.
3. Recipient's
Catalog
No.
NASA CP-3099 4. Title
5. Report
and Subtitle
Multisource
Data
Integration
in Remote
Date
January
Sensing
6. Performing
1991 Organization
Code
Organization
Report
930 8. Performing
7. Author(s)
James
C. Tilton, Editor
90B00122 10. Work
9. Performing
Organization
Name
Unit
Flight
Agency
Name
of Report
Conference
and Address
National Aeronautics and Space Washington, DC 20546-0001
15. Supplementary
or Grant
No.
Center 13. Type
12. Sponsoring
No.
and Address 11. Contract
NASA Goddard Space Greenbelt, MD 20771
No.
and Period
Covered
Publication
Administration 14. Sponsoring
Agency
Code
Notes
This workshop was organized by Recognition and co-sponsored Goddard Space Flight Center, Geoscience and Remote Sensing
Technical Committee 7 of the International Association for Pattern by the Space Data and Computing Division (Code 930) of the and by the Washington/Northern Virginia Chapter of the IEEE Society.
16. Abstract
Multisource
Data
instruments
and new sensors
huge amount
Integration
support during
integration
This
and increase
system
FORM
This
1626 OCT 86
observations and
while
model
from
different
can be identified
sessions
to five individual
of this world.
properties Multiple
contradictions
a valid source
of three
of three
and in the general Publication, along
(and
independent)
may be caused
as such.
of information
But also,
are is among the sources may give data
by noise,
As a consequence, for any geographical
presentations.
- Unlimited
Subject Classif.
Unclassified
(of this page)
21.
Category
No. of pages
164
43 22.
were
papers
Statement
Unclassified
20. Security
All papers
context of the session. The full text of these with three workshop summary papers. 18. Distribution
by Author(s))
(of this report)
Unclassified NASA
New
of the "real world."
(GIS).
consisted
(Suggested
Classif.
in the near future.
of new views
and they represent
Multisource Data Integration Remote Sensing Geographic Information Systems Ground Reference Data Image Registration 19. Security
a real challenge
in a (computer-)
their credibility,,
or misinterpretations,
are very reliable
both individually in this Conference
17. Key Words
and integrated
of the world--consistent
processing,
workshop
discussed included
views each other
results
information
will become
us with a large variety
of how these data are gathered and what their characteristic of information that contribute to a meaningful interpretation.
us complementary errors
Sensing
of data has to be combined
the knowledge useful sources sources
in Remote will provide
Price
A08
is
....
U" ----
,]_'r'--=
_
_--_i
__?_
..........
-= = :.:,2-_. _=?------
_F::,
¸
.