logging in or signing up Satellite retreival of AOT over Desert regions aSGuest169 Download Post to : URL : Related Presentations : Share Add to Flag Embed Email Send to Blogs and Networks Add to Channel Uploaded from authorPOINT lite Insert YouTube videos in PowerPont slides with aS Desktop Copy embed code: (To copy code, click on the text box) Embed: URL: Thumbnail: WordPress Embed Customize Embed The presentation is successfully added In Your Favorites. Views: 127 Category: Entertainment License: All Rights Reserved Like it (1) Dislike it (0) Added: September 25, 2008 This Presentation is Public Favorites: 0 Presentation Description No description available. Comments Posting comment... Premium member Presentation Transcript Satellite Retrieval of AOT over Desert Regions : Satellite Retrieval of AOT over Desert Regions Wolfgang von Hoyningen-Huene, John P. Burrows, Institute of Environmental Physics, University of Bremen _________ AOD retrieval validation Over deserts – no regular AOD products only TOMS AAI Aim: extension of BAER for desert conditions Validation of retrieved AOD Determination of AOT : Determination of AOT BAER (Bremen AErosol Retritrival) is used for spectral AOT < 0.67 µm over land Clouds separately treated by the asymptotic theory for optically thick clouds (A. Kokhanovsky) -> COT Angström derived from spectral AOT AOT(0.412 µm) + use for the determination of additional aerosol parameters Reff and NAER. Adaptations for desert conditions required Retrieval Requirements : From radiative transfer equation one obtains the aerosol reflectance Aerosol parameters Surface reflectance Retrieval Requirements Comparison of Phase Functions : Comparison of Phase Functions Models underestimate lateral scattering Surface Reflectance : Surface Reflectance Desert cases Now implemented Status : Status Aerosol parameters: Europe: phase function + SSA from LACE-98 Desert: phase function (Senegal 1995) future: phase function + SSA from SAMUM OPAC overestimates AOT Surface reflectance: Europe: vegetation mix tuned by NDVI Desert: now: static bright soil spectrum (F. Baret, INRA) future: a) data base from C. Hsu (NASA) b) model derived from SAMUM MERIS AOD L3 ACRI : MERIS AOD L3 ACRI Satellite Properties 1 : Satellite Properties 1 Observation data Spectral Channels 1 : Spectral Channels 1 UV channels Solar IR Spectral Channels 2 : Spectral Channels 2 Coverage 1 : SeaWiFS daily coverage (Clorophyll product, from GAC L1b data ) Swath width: 2400 km Morocco: every 1 - 2 days Coverage 1 ENVISAT Meris: Swath width: 1100 km (only the half) SCIAMACHY: 980 km AATSR: 512 km Coverage about every 2 days Coverage 2 : Coverage 2 TOMS: 2800 km swath, total coverage, every day Coverage 3 : Coverage 3 MODIS: Swath 2330 km Data Access + Availability : Data Access + Availability Ground Measurements : Ground Measurements Cloud free conditions: Sun photometer: AOD(), 7 channels, CIMEL 318 1.020, 0.870, 0.670, 0.500, 0.440, 0.380, 0.340 Cloud free + zo > 60° Skyradiometer: LSky(, zo, ) ALMU, 4 (7 ?) channels, CIMEL (LSky(, z, o) PPL, 4 channels, CIMEL) p(), o by CIRATRA Old ASP 4 photometer: Surface Reflectance (, zo, ) Totally cloudy or homogeneous Ci: Skyradiometer LSky(, z, o) PPL, 4 channels, CIMEL cos(z)*Cloud LSky(, zo, ) ALMU, 4 channels, CIMEL pCi() Instruments : ASP-5 CIMEL 318 Instruments Data Examples : Data Examples Preparation : Preparation Investigation of the temperature influence of the CIMEL Langley-plots, Zugspitze + Bremen Improvment of Calibration check: Calibration campaign at Zugspitze in March 2005 Reference of the sky channels (aureole + sky) to the solar channel (for o required) Additional blocking of channel 7 and 8 (0.380 + 0.340 µm) Leakage light from double wavelength You do not have the permission to view this presentation. In order to view it, please contact the author of the presentation.
Satellite retreival of AOT over Desert regions aSGuest169 Download Post to : URL : Related Presentations : Share Add to Flag Embed Email Send to Blogs and Networks Add to Channel Uploaded from authorPOINT lite Insert YouTube videos in PowerPont slides with aS Desktop Copy embed code: (To copy code, click on the text box) Embed: URL: Thumbnail: WordPress Embed Customize Embed The presentation is successfully added In Your Favorites. Views: 127 Category: Entertainment License: All Rights Reserved Like it (1) Dislike it (0) Added: September 25, 2008 This Presentation is Public Favorites: 0 Presentation Description No description available. Comments Posting comment... Premium member Presentation Transcript Satellite Retrieval of AOT over Desert Regions : Satellite Retrieval of AOT over Desert Regions Wolfgang von Hoyningen-Huene, John P. Burrows, Institute of Environmental Physics, University of Bremen _________ AOD retrieval validation Over deserts – no regular AOD products only TOMS AAI Aim: extension of BAER for desert conditions Validation of retrieved AOD Determination of AOT : Determination of AOT BAER (Bremen AErosol Retritrival) is used for spectral AOT < 0.67 µm over land Clouds separately treated by the asymptotic theory for optically thick clouds (A. Kokhanovsky) -> COT Angström derived from spectral AOT AOT(0.412 µm) + use for the determination of additional aerosol parameters Reff and NAER. Adaptations for desert conditions required Retrieval Requirements : From radiative transfer equation one obtains the aerosol reflectance Aerosol parameters Surface reflectance Retrieval Requirements Comparison of Phase Functions : Comparison of Phase Functions Models underestimate lateral scattering Surface Reflectance : Surface Reflectance Desert cases Now implemented Status : Status Aerosol parameters: Europe: phase function + SSA from LACE-98 Desert: phase function (Senegal 1995) future: phase function + SSA from SAMUM OPAC overestimates AOT Surface reflectance: Europe: vegetation mix tuned by NDVI Desert: now: static bright soil spectrum (F. Baret, INRA) future: a) data base from C. Hsu (NASA) b) model derived from SAMUM MERIS AOD L3 ACRI : MERIS AOD L3 ACRI Satellite Properties 1 : Satellite Properties 1 Observation data Spectral Channels 1 : Spectral Channels 1 UV channels Solar IR Spectral Channels 2 : Spectral Channels 2 Coverage 1 : SeaWiFS daily coverage (Clorophyll product, from GAC L1b data ) Swath width: 2400 km Morocco: every 1 - 2 days Coverage 1 ENVISAT Meris: Swath width: 1100 km (only the half) SCIAMACHY: 980 km AATSR: 512 km Coverage about every 2 days Coverage 2 : Coverage 2 TOMS: 2800 km swath, total coverage, every day Coverage 3 : Coverage 3 MODIS: Swath 2330 km Data Access + Availability : Data Access + Availability Ground Measurements : Ground Measurements Cloud free conditions: Sun photometer: AOD(), 7 channels, CIMEL 318 1.020, 0.870, 0.670, 0.500, 0.440, 0.380, 0.340 Cloud free + zo > 60° Skyradiometer: LSky(, zo, ) ALMU, 4 (7 ?) channels, CIMEL (LSky(, z, o) PPL, 4 channels, CIMEL) p(), o by CIRATRA Old ASP 4 photometer: Surface Reflectance (, zo, ) Totally cloudy or homogeneous Ci: Skyradiometer LSky(, z, o) PPL, 4 channels, CIMEL cos(z)*Cloud LSky(, zo, ) ALMU, 4 channels, CIMEL pCi() Instruments : ASP-5 CIMEL 318 Instruments Data Examples : Data Examples Preparation : Preparation Investigation of the temperature influence of the CIMEL Langley-plots, Zugspitze + Bremen Improvment of Calibration check: Calibration campaign at Zugspitze in March 2005 Reference of the sky channels (aureole + sky) to the solar channel (for o required) Additional blocking of channel 7 and 8 (0.380 + 0.340 µm) Leakage light from double wavelength