notes and correspondence - Geophysical Fluid Dynamics Laboratory
Recommend Documents
Geophysical Fluid Dynamics Laboratory/NOAA, Princeton University, Princeton, New Jersey. 19 April ... timated using the monthly âZurichâ sunspot numbers.
Oct 31, 2014 - bootstrap resampling upon the original .... seasonal SST grids were converted to anomalies, ..... noaa.gov/psd/data/gridded/data.gpcp.html).
Nov 1, 1985 - A more direct proof of orthogonality is also available. The eigenvalue equation .... If we add a small scale-selective damp- ing of vorticity to the ...
6S 6 68. 62[(KH+ as) 62] (3) where t is time and z the vertical coordinate; z = 0 will ..... of the proï¬le on a vertical plane normal to the ice leading edge. The.
May 5, 1975 - Q. 90 60/ ,-. \l/ 1897 @D i so\ 336 10 Boï¬/ï¬o \~IO LE. 7 2o \ I .500â ..... holding capacity of the model atmosphere with time. In order to economize ...
5 a 0.4 0.4. 0.1 0.2 0.21 of f .i o i. 0 5 10 15 20 25 50 5 1o 15 20 25 50. 1.2 1.2 m 1< b 1. 0 Z5-55ï¬,5â15N ZWW.7â15N. 3 00+ 00+. 3 0.0 0.0. 5 g, 0.4 o.4~ h].
... water masses from which it originated. This level of saliniï¬cation is nowhere near the 0.9 unit in ...... SON SON 30N E0 303 505. 2000;. 3000â 5. ' DEPTH (m).
MONTHLY WEATHER REVIEW ... and Oceanic Sciences, Princeton University, Princeton, New Jersey .... climatological monthly mean SST data were used. By.
6S 6 68. 62[(KH+ as) 62] (3) where t is time and z the vertical coordinate; z = 0 will ..... of the proï¬le on a vertical plane normal to the ice leading edge. The.
Nov 15, 1989 - worth and McIntyre 1.985, for a review of critical layer theory). One is led to the hypothesis that the existence of a simple asymmetric life cycle of ...
the descending branch of Hadley cell and dry air ad- vecting out from the colder continent. Although ECHAM4 qualitatively simulates most of the above features, ...
Jan 4, 1996 - Geophysical Fluid Dynamics Laboratoty/NOAA, Princeton, New Jersey. (Manuscript .... The GFDL dataset of monthly mean variables and.
AVHRR channel spectral responses and descriptions (after Kidwell 1991). Central wavenumber. (cm'). Central wavelength. (microns). Approximate peak in.
Sigma Coordinate Pressure Gradient Errors and the Seamount Problem ... gradients on a sigma coordinate grid, prognostically disappeared, leaving behind a ...
thickness of isopycnal layers (e.g., Marshall 1997). Ana- lyzing the circulation in density space essentially elimi- nates the northern downwelling branch of the ...
Oct 1, 1992 - guidance as to the dependence on temperature gra- vertical shear, (U(H) â U(0))/H. .... In the absence of the damping terms, baroclinic insta-.
Curriculum Vitae: Venkatramani BALAJI. Contact information .... DeLuca, C., G.
Theurich, and V. Balaji, 2012: The Earth System Modeling Framework. Earth.
George J. Boer and Francis Zwiers. Canadian Centre for Climate Modelling and Analysis, ... Jason Bell. David Karoly. University of California, Santa Cruz, Santa ...
Nov 29, 2005 - Geophysical Fluid Dynamics Laboratory, Princeton, New Jersey, USA ... present-day monthly mean aerosol climatologies are generated from ...
Jan 15, 1995 - (Manuscript received 27 April 1993, in ï¬nal form 6 June 1994). ABSTRACT ..... [or equivalently LSE for S6 = 6A + (l â e)B] for values of 6 ...
May 1, 1996 - the contamination of the global tidal signal by regional search Center ..... or ~25 km) following the second 1977 dust storm (Ls jet strengthens.
Comprehensive, coupled ocean-atmosphere GCMs for the culty of the Surface ..... The albedos of snow cover and sea ice were assumed ... Snot ungmt.
quences for the World Ocean circulation, as first from lower latitudes. A sharp density gradient between emphasized by Gill and Bryan (1971). Antarctic waters ...
notes and correspondence - Geophysical Fluid Dynamics Laboratory
Mar 3, 1993 - NOAA, Princeton University, P.O. Box 308, Princeton, NJ 08542. NH lower ... The phase of the QBO was characterized using the monthly mean.