PPT-Assimilation and Evaluation of MISR Cloud Tracked Winds wit

Junjie Liu 1 and Kevin Mueller 1 1 Jet Propulsion Lab JPL Caltech With special thanks to Joe Stassi GMAO Dan Holdaway GMAO Meta Sienkiewicz GMAO Will McCarty GMAO Ron . Whereas the fixed receiver technology is in promotion for last many years and about 70 systems covering over 20000 sq m of dish area have been installed the fully tracked technology is under pilot scale demonstration and only 10 dishes with area 1 6 Science Advisory Committee Meeting. 26 – 28 August, 2014. National Space Science and Technology Center, Huntsville, AL. Introduction. SPoRT assimilates AIRS, CrIS, and IASI profiles into regional models to demonstrate their impact on NWP and address specific forecast issues. Will McCarty. NASA Goddard Space Flight Center. Global Modeling and Assimilation Office. 2015 JCSDA Workshop. 14 May 2015. Introduction. Traditionally, only those infrared radiance observations which are unaffected by clouds are assimilated. Michele . Rienecker. Global Modeling and Assimilation Office. NASA/GSFC. WMO CAS Workshop. Sub-seasonal to Seasonal Prediction. Met Office, Exeter. 1 to 3 December 2010 . 2. What do we mean by “coupled data assimilation”?. Benjamin Ruston. Steve Swadley, Nancy Baker, . Rolf . Langland. NRL, . Monterey, . CA. Outline. Gather information about instrument: . What are previous sensors or instruments, how have they been used?. 2: Racial and Ethnic Relations. Assimilation. Assimilation. . is a process in which formerly distinct and separate groups come to share a common culture and merge together socially. . As a society undergoes assimilation, differences among groups begin to decrease.. Gregory Carmichael(1), . Pablo . E. . Saide. (NCAR), . Meng. . Gao. (1), Maryam . Abdioskouei. (1), . Arlindo da Silva (NASA GSFC), R. Brad Pierce (NOAA NESDIS-STAR), David G. Streets (ANL), . Jhoon. Kevin Garrett. 1,2,3. , Sid Boukabara. 1,2. , . and Erin Jones. 1,2,3. 1. NOAA/NESDIS/STAR. 2. Joint Center for Satellite Data Assimilation. 3.. Riverside Technology, Inc.. Preparation for GPM GMI . . Active Aerosol Plume-Height (AAP) Project . 9 November 2018. Stereo images from NASA’s Multi-Angle Imaging Spectroradiometer (. MISR. ) make it possible to map plume heights in ongoing eruptions using parallax in the stereo imagery. We can also distinguish eruptive plumes from metrological clouds and remobilized ash with these data, based on retrieved plume height, retrieved particle properties, and feature texture and . Source https//supportofficecom1Review accept reject and hide tracked changesin Microsoft WordApplies ToWord 2010Word 2007To prevent you from inadvertently distributing documents that contain tracked c . VIIRS Snow . and . Ice Product Provisional Maturity Review November 14, 2013. Mike . Ek. , . Jiarui. Dong . and EMC Land Team. NOAA/NCEP/EMC. •. Unified Noah LSM in all NCEP NWP and climate systems, plus in NLDAS/GLDAS.. in the NCEP Global Forecast System. 1. Ting-Chi Wu. 1. , Lewis Grasso. 1. , . Milija. Zupanski. 1. , Heather Cronk. 1. , . James Fluke. 1. , Richard Schulte. 2. , Wesley Berg. 2. , Anton Kliewer. 1. Global . Winds. - A . current. is a flow of air or water in a certain direction.. Global . Winds. Winds move from areas of . high. pressure to . low. pressure.. You might expect them to move straight from the poles (high pressure) to the equator (low pressure)but…. Local winds are caused by the movement of air between low-pressure and high-pressure systems within small areas. As there are so many different types of winds, each one takes on a unique form. Local winds frequently have a significant impact on climate in local regions, so it is critical to understand what causes them..