PDF-THE VALIDATION OF AEROSOL OPTICAL THICKNESS RETRIED BY BAND CORRELATIO
Author : celsa-spraggs | Published Date : 2016-07-24
Y Kawata H Fukui and K Takemata Earth and Social Information Core Dept of Computer Science Kanazawa Institute of Technology Japan kawatainforkanazawaitacjp KEY
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THE VALIDATION OF AEROSOL OPTICAL THICKNESS RETRIED BY BAND CORRELATIO: Transcript
Y Kawata H Fukui and K Takemata Earth and Social Information Core Dept of Computer Science Kanazawa Institute of Technology Japan kawatainforkanazawaitacjp KEY WORDS Remote Sensing. VIIRS Aerosol Cal/Val Team. VIIRS Aerosol Science and Operational Users Workshop November 21-22, 2013. 1. Outline. VIIRS Aerosol Products. Environmental Data Record (EDR). Intermediate Product (IP). Jingqiu . Mao . (GFDL/NOAA), . Songmiao. Fan (. GFDL/NOAA), . Ying . Chen (. Fudan. U, China). A . dominant source of nutrient iron to open . ocean, critical for plankton in surface waters:. -Biological pump of CO2. Betty Croft. 1. , Jeff Pierce. 1,2. and Randall Martin. 1,3. 1. Dalhousie University, Halifax, Canada. 2. Colorado State University, Fort Collins, USA. 3. Harvard-Smithsonian Center for Astrophysics, Cambridge, USA. Yan . Zhang. 1. , . Hongbin. . Yu. 2. , . Alexander . Smirnov. 1. , . Tom . Eck. 1. , . Mian. . Chin. 3. , . Lorraine . Remer. 3. , . Qian. . Tan. 1. , . Robert . Levy. 4. 1 GESTAR/USRA, 2 ESSIC, 3 NASA/GSFC, 4 SSAI. An Introduction to Aerosol Propellants 3 Aerosol Product System 4 Aerosol Product System 5 Aerosol Product System 6/MCI; 8 ;/MCI; 8 ;Aerosol Product System 7 Aerosol Product System 8 A 2. Column Retrievals with Ground-based Monitors. Randall . Martin (Dalhousie, Harvard-Smithsonian). with . contributions from. Melanie Hammer, . Shailesh. . Kharol. , Jeff Geddes (Dalhousie U). TEMPO Science Team Meeting. Jacob Anderson. Mentor: Gregory . Leptoukh. Research Objectives. Based on previous research determine the variables that most affect MODIS bias. Find which MODIS aerosol algorithm works better over coastal regions. . . C. Jordan. 1. , B. Anderson. 2. , A. . Beyersdorf. 2. , . J. Dibb. 1. , M. Greenslade. 1. , R. Martin. 2. , E. Scheuer. 1. , L. Thornhill. 2. , D. Troop. 1. , E. Winstead. 2. , and L. Ziemba. 2. Optical Position sensor (Finishing). Diamond Detector for . Secondaries. (Starting). Meeting - Wire Scanner Electronics . 15/03/2013. Jose Luis . Sirvent. PhD. Student. 1. Optical Position Sensor. A)Electronics (Schematic):. eulerian. model WRF/. Chem. Paolo Tuccella, Gabriele Curci, . Suzanne. . Crumeyrolle. , Guido Visconti. Direct and . Indirect. aerosol . effects. Clean. Polluted. Direct . effect. Indirect. . effect. Betsy Berry and Jay Mace. University of . Utah. American Geophysical Union 2011 . Fall Meeting. More CCN→. more small droplets→ . less collision→ delayed raindrop formation . Smaller sizes are lofted higher where they freeze→ latent heat release leads to increased buoyancy and a stronger updraft. Robert Wood, Atmospheric Sciences,. University of Washington. Motivation. Aerosols can potentially influence earth’s radiation budget both by direct interaction with sunlight (aerosol . direct . effect), and also by altering cloud radiative properties (aerosol . Jón. Egill . Kristjánsson. (Univ. Oslo). Many thanks to: Alf . Kirkevåg. (. met.no. ), . Corinna. . Hoose. (Univ. Oslo), Leo Donner (GFDL). Problem Definition. Most GCMs give an aerosol indirect effect which is too high compared to results from residual calculations – . Betsy Berry and Jay Mace. University of . Utah. American Geophysical Union 2011 . Fall Meeting. More CCN→. more small droplets→ . less collision→ delayed raindrop formation . Smaller sizes are lofted higher where they freeze→ latent heat release leads to increased buoyancy and a stronger updraft.
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