PDF-AIRS/AMSU/HSB Version 5 Data Release User Guide Page 1 AIRS/AMSU/HSB

June 2007 Version 10 Jet Propulsion Laboratory California Institute of Technology Pasadena CA Submit Questions to httpairsjplnasagovAskAirs AIRSAMSUHSB Version 5 Data Release User Guide. AIRS/AMSU/HSB Version 6 Retrieval Flow Page AIRS/AMSU/HSB Version 6 Retrieval Flow Page INTRODUCTION TO V6 RETRIEVAL FLOW All quantities marked best (associated quality factor = 0) and almost all ARSET. A. pplied. . R. emote. . S. E. nsing. . T. raining. CO plumes at an altitude of roughly 2 km (700 . millibars. ) over the Houston area and extending out over the Bay of Galveston. This image represents a composite of data collected over a 10-day period, September 6-15, 2002, by MOPITT.. Computer-Based Testing (CBT). AIRS Webinar: October 2013. The Original Way. AIRS Certification has been around for over 15 years. Eligible candidates take a 100 question exam and acquire either CIRS, CIRS-A or CRS Certification if they pass the exam. 1. , Eric Stevens. 1. , Xiangdong Zhang. 1. ,Tom Heinrichs. 1. , Scott Macfarlane. 1. , Don Morton,. 2. Melissa Kreller. 3. , and Bradley Zavodsky. 4. . Affiliations:. 1 . Geographic Information Network of Alaska, UAF. Bradley Zavodsky. 1 . , Danielle Kozlowski. 2. 1. NASA Short-term Prediction Research and Transition (SPoRT) Center, Huntsville, Alabama. 2. Soil, Environmental and Atmospheric Science Department, University of Missouri, Columbia, Missouri. Development of Observing System Simulation Experiments . for all-sky radiance data assimilation at NASA GMAO. Min-Jeong Kim. NASA GMAO/GESTAR. Collaborators: Ricardo Todling, Will McCarty, Ron Gelaro, Ron Errico, Nikki Prive, Jong Kim, Dan Holdaway, Jianjun Jin, and Wei Gu. Introduction. The Arctic Region Supercomputing . Center. has been running a quasi-operational prototype of a High Resolution Rapid Refresh for Alaska (HRRRAK) at 3km resolution, initialized by the 13km Rapid Refresh (RR). Although the RR assimilates a broad range of observations into its analyses, preliminary experiments with the HRRRAK suggest that there may . Carl Mears. Remote Sensing Systems. Why do we care about . the diurnal cycle?. Most polar orbiting satellites drift in local measurement time – need estimate of diurnal cycle to adjust for this.. Model validation studies. Ralph . Ferraro. 1. . (Ralph.R.Ferraro@noaa.gov), . Chi Quinn. 1,2. . a. nd Daniel Cecil. 3. 1. NOAA/NESDIS/. Center. . for Satellite Applications and Research (STAR), College Park, . MD. 2. American University, Washington, DC. (LANCE). GES DISC UWG. May 10-11, 2011. Karen Michael. EOSDIS System Manager. Karen.Michael@nasa.gov. 301-614-5286. 1. What is LANCE?. LANCE was initiated by the NASA Flight, Research, and Applied Sciences Programs in order to ensure the availability of NASA satellite data products to those partners who have grown to rely upon NASA for data for their decision support systems.. . Satellite Application Facility on Support to Operational Hydrology and Water Management . Ten . Gars. Stefania De Angelis. was established by the EUMETSAT Council on 3 July 2005 as part of the. . Ralf Bennartz . AOS/CIMSS/SSEC. University of Wisconsin – Madison. Outline. What we want to know and why we need it?. What does a satellite really observe (a.k.a. The radiative transfer equation). Weighting functions. -NPP. Joel Susskind. NASA GSFC Sounder Research Team (SRT). Suomi. -NPP Workshop. June 21, 2012. Washington, D.C.. National Aeronautics and Space Administration. www.nasa.gov. . Joel . Susskind. Andrew Collard. IMSG@NOAA/NCEP/EMC. JPSS/GOES-R Risk Reduction Summit . Radiance Data Used in the . NCEP Global Model. JPSS/GOES-R Risk Reduction Summit . Microwave:. AMSU-A. : NOAA-15, 18, 19, . MetOp.