PPT-Cloud/Rain partitioning using MODIS and AMSR-E

Author : test | Published Date : 2016-03-29

Matt Lebsock Aqua AMSR E amp MODIS Drizzle defined where 750 meter reflectivity exceeds 15 dBZ Area and Low cloud fraction weighted oceanic mean is 192 The world

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Cloud/Rain partitioning using MODIS and AMSR-E: Transcript

Matt Lebsock Aqua AMSR E amp MODIS Drizzle defined where 750 meter reflectivity exceeds 15 dBZ Area and Low cloud fraction weighted oceanic mean is 192 The world is a drizzly place The water path can be partitioned between cloud and Precipitation. CloudSat. Matt . Lebsock. Chris . Kummerow. Motivation. Radiosonde. data [. Ohtake. , 1963. ]. Warm rain falls in all tropical ocean basins in all seasons more frequently than expected. Shipboard Weather Reports [. C. ollection 6 Ice . M. odel . A. ssessments with POLDER and CALIPSO. Ping Yang, . Souichiro. . Hioki. , . Jiachen. Ding . Department of Atmospheric . Sciences. Texas A&M University. In collaboration with . stratocumulus clouds and . drizzle. Sandra . Yuter. Department of Marine, Earth, and Atmospheric Sciences. North Carolina State . University. May 2011. Stratocumulus formation. Stevens 2005, from Arakawa 1975. Photograph: Tony Clarke, VOCALS . REx. flight RF07. Robert Wood. University of Washington. “Background” cloud droplet concentration critical for determining aerosol indirect effects. Quaas. et al., AEROCOM . Jean-Luc . Moncet. P. Liang, J. Galantowicz, G. Uymin, A. Lipton, C. Prigent*, B. Hornbuckle**. Atmospheric and Environmental Research, . Inc.. *LERMA. **Iowa State University. First version of global monthly. AMSR-E and WindSat Ocean Products. Frank . J. . Wentz. Remote Sensing Systems, Santa Rosa CA. AMSR TIM Agenda. 4-5 September . 2013. Mandalay Beach, CA. Retrieve accurate wind speeds when rain is present. Zhibo (. zippo. ) Zhang. 03/29/2010. ESSIC. Outline. Background. Importance of ice cloud. Ice particle model and ice cloud retrieval. Influence of ice particle model on . t. retrieval. Comparison of MODIS and POLDER ice .  VIIRS AOD. Robert Levy. . (NASA-GSFC). Shana . Mattoo. , Leigh . Munchak. . (SSAI @ NASA-GSFC). Falguni. . Patadia. (GESTAR/Morgan State Univ. @ NASA-GSFC). Lorraine Remer (JCET-UMBC). VIIRS-2013 College Park, MD, November 2013. ATM 419/563. Spring 2017. Fovell. 1. The C-C equation. The . Clausius-Clapeyron. (C-C) . equation reveals how saturation . vapor pressure (. e. s. ) varies . with temperature . T. :. …where . a. 1. Jean-Luc . Moncet. P. Liang, J. Galantowicz, G. Uymin, A. Lipton, C. Prigent*, B. Hornbuckle**. Atmospheric and Environmental Research, . Inc.. *LERMA. **Iowa State University. First version of global monthly. AMSR-E and WindSat Ocean Products. Frank . J. . Wentz. Remote Sensing Systems, Santa Rosa CA. AMSR TIM Agenda. 4-5 September . 2013. Mandalay Beach, CA. Retrieve accurate wind speeds when rain is present. Andrew M. Sayer, N. Christina Hsu, Corey Bettenhausen, Myeong-Jae . Jeong, Jaehwa Lee. MODIS . Red. -. Green. -. Blue. composite. MODIS . Dark. Target . AOD. 0. 0.5. 1.0. 1.5. 2.0. MODIS . Deep. Blue AOD. M. odel . A. ssessments with POLDER and CALIPSO. Ping Yang, . Souichiro. . Hioki. , . Jiachen. Ding . Department of Atmospheric . Sciences. Texas A&M University. In collaboration with . Steven . about 1000 m/48 hrs. Thus, they usually evaporate quickly upon leaving the cloud mass. . For it to fall as a raindrop the cloud droplet must get bigger. One raindrop = about 1 million cloud droplets, .

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