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2. Jan Cermak, ETH Zurich. NETFAM/EG-CLIMET Oslo, 3/2009. Optimum Observation Strategies. □ Goal: High-Resolution Climate/Weather Analysis.
Ground-Based and Satellite Remote Sensing for Atmospheric Analysis Jan Cermak, ETH Zurich

Optimum Observation Strategies  Goal: High-Resolution Climate/Weather Analysis  Accurate  Reliable  Complete

→ System integration!

NETFAM/EG-CLIMET Oslo, 3/2009

Jan Cermak, ETH Zurich

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Outline 1. A Spatial Problem: Characterizing the Atmosphere 2. Looking for Truth: Ground-Based RS as a Reference 3. The Big Picture: Multi-Perspective Remote Sensing

NETFAM/EG-CLIMET Oslo, 3/2009

Jan Cermak, ETH Zurich

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Outline 1. A Spatial Problem: Characterizing the Atmosphere 2. Looking for Truth: Ground-Based RS as a Reference 3. The Big Picture: Multi-Perspective Remote Sensing

NETFAM/EG-CLIMET Oslo, 3/2009

Jan Cermak, ETH Zurich

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1. RS for Model Evaluation  COST 722 3D Fog Model Intercomparison  Lindenberg, Germany, September-December 2005  4 European 3D models

 Evaluation  Correct detection of fog presence  Correct representation of atmospheric properties

NETFAM/EG-CLIMET Oslo, 3/2009

Jan Cermak, ETH Zurich

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1. RS for Model Evaluation

Radiosonde: dashed black, Lindenberg, Germany, 7 Dec 2005 (Masbou 2008) NETFAM/EG-CLIMET Oslo, 3/2009

Jan Cermak, ETH Zurich

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1. RS for Model Evaluation

COSMO-FOG, Lindenberg, Germany, 26 Sep 2005 (Masbou 2008) NETFAM/EG-CLIMET Oslo, 3/2009

Jan Cermak, ETH Zurich

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1. RS for Model Evaluation

COSMO-FOG, Lindenberg, Germany, 26 Sep 2005 (Masbou 2008) NETFAM/EG-CLIMET Oslo, 3/2009

Jan Cermak, ETH Zurich

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1. RS for Model Evaluation

NMM-PAFOG, Zurich Airport, Switzerland, 11 Oct 2005 (Müller 2006) NETFAM/EG-CLIMET Oslo, 3/2009

Jan Cermak, ETH Zurich

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1. RS for Model Evaluation  Conclusions Model Intercomparison  Detection of feature presence not enough  Spatial component is part of good forecast  Reliable spatial observations essential

NETFAM/EG-CLIMET Oslo, 3/2009

Jan Cermak, ETH Zurich

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Outline 1. A Spatial Problem: Characterizing the Atmosphere 2. Looking for Truth: Ground-Based RS as a Reference 3. The Big Picture: Multi-Perspective Remote Sensing

NETFAM/EG-CLIMET Oslo, 3/2009

Jan Cermak, ETH Zurich

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Feature Presence

NETFAM/EG-CLIMET Oslo, 3/2009

Jan Cermak, ETH Zurich

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Feature Presence: Helsinki Test Bed

NETFAM/EG-CLIMET Oslo, 3/2009

Jan Cermak, ETH Zurich

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Vertical Information: TUC Campaign, 2003/2004 6/12/2003: Radar reflectivity, LWP and cloud thickness

Cermak et al. 2006 (Met. Z.)

NETFAM/EG-CLIMET Oslo, 3/2009

Jan Cermak, ETH Zurich

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Satellite-Derived Parameters: Cloud Water

NETFAM/EG-CLIMET Oslo, 3/2009

Jan Cermak, ETH Zurich

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Satellite-Derived Parameters  Cloud properties    

Radiance, temperature, reflectance Geometry: height, thickness Optics: optical thickness Microphysics: liquid water path/content, effective droplet radius

 Aerosol properties  (parameters similar to clouds)

 Others  Water vapour (precipitable water)  ...

NETFAM/EG-CLIMET Oslo, 3/2009

Jan Cermak, ETH Zurich

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Outline 1. A Spatial Problem: Characterizing the Atmosphere 2. Looking for Truth: Ground-Based RS as a Reference 3. The Big Picture: Multi-Perspective Remote Sensing

NETFAM/EG-CLIMET Oslo, 3/2009

Jan Cermak, ETH Zurich

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Low stratus Europe, 10/2008  Step 1: Ground-based assessment

Data: Linden, Germany, courtesy U Marburg NETFAM/EG-CLIMET Oslo, 3/2009

Jan Cermak, ETH Zurich

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Low stratus Europe, 10/2008  Step 2: Transect analysis (active sensor satellite)

Fiures: CALIPSO Science Team NETFAM/EG-CLIMET Oslo, 3/2009

Jan Cermak, ETH Zurich

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Low stratus Europe, 10/2008  Step 3: Spatial component (passive sensor satellite)

Figures: Products based on Meteosat 9 SEVIRI data NETFAM/EG-CLIMET Oslo, 3/2009

Jan Cermak, ETH Zurich

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Low stratus Europe, 10/2008  Step 3: Spatial component (passive sensor satellite)

Figures: Products based on Meteosat 9 SEVIRI data NETFAM/EG-CLIMET Oslo, 3/2009

Jan Cermak, ETH Zurich

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Low stratus Europe, 10/2008  Step 4: Validation/ Joint analysis

NETFAM/EG-CLIMET Oslo, 3/2009

Jan Cermak, ETH Zurich

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Conclusions  Ground-based and satellite systems are complementary  Algorithm development profits from data comparison  Joint interpretation/joint products → to be discussed in WG4

NETFAM/EG-CLIMET Oslo, 3/2009

Jan Cermak, ETH Zurich

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