PPT-JCSDA OSSEs for Geostationary

Hyperspectral IR and MW Sean PF Casey 12 Narges Shahroudi 12 Jack Woollen 3 Sid Boukabara 2 Kayo Ide 1 Ross Hoffman 4 and Robert Atlas 5 1 ESSICUMD 2 NOAANESDISSTARJCSDA . By Tom,is Soler, 1 Member, ASCE, and David W. Eisemann-' ABSTRACT: geodetic theory is applied to determine the geodetic azimuth and geodetic altitude required to point dish antennas to geostationary Settler. What is this picture of ?. Learning Objectives. To know what a satellite is. To know some uses of artificial satellites. To understand the differences between polar and geostationary . orbits and where they are used. David Edwards (NCAR) and . Arlindo. . D. eSilva. (NASA GSFC). . with input from the GEO. -CAPE SWG . CEOS/MACC-II OSSE Workshop. A global GEO OSSE activity for GEO-CAPE & CEOS. Motivation. : NASA . The GOES - R Series: - Generation Geostationary Weather Satellites Greg Mandt GOES - R System Program Director 28th Annual Glen Gerberg Weather and Climate Summit January 13, 2015 Our mission is Lecture 1: Theory. Steven J. Fletcher. Cooperative Institute for Research in the Atmosphere. Colorado State University. Overview of Lecture. Motivation. Evidence for non-Gaussian . Behaviour. Distributions and Descriptive Statistics . What Is an Orbit?. Johannes . Kepler. discovered (in . 1600s. ) that planets orbit in . ellipses, . not . circles.. Satellites (natural or . human-made. ) also orbit Earth in elliptical . pattern.. Elliptical orbits remain fixed in space and Earth spins under a fixed satellite . Unit 2 . Content . Introduction . Antenna . Look . Angels. The . Polar Mount Antenna . Limits . of . Visibility. Near . Geostationary Orbits . Earth . Eclipse of . Satellite. Sun . Transit Outage . Launching . Hyperspectral. -IR and MW. Sean PF Casey. 12. , . Narges. Shahroudi. 12. , Jack Woollen. 3. , Sid . Boukabara. 2. , Kayo Ide. 1. , Ross Hoffman. 4. , and Robert Atlas. 5. 1. ESSIC/UMD . 2. NOAA/NESDIS/STAR/JCSDA . Sean PF Casey. 1,2. , Ross N. Hoffman. 1,2. , Robert Atlas. 2. , and Lidia Cucurull. 2. 1. Cooperative Institute for Marine and Atmospheric Studies/University of Miami. 2. NOAA/OAR/Atlantic Oceanographic and Meteorological Laboratory. Lidia Cucurull. . (*)(**) . Chief, Global Observing Systems Analysis (GOSA) Group. Ruifang. Li. (*). , . Hongli. Wang. (*. ). , Jason English. (*). , . Tanya . Peevey. (*). , and Kirk . Holub. (*). Science Workshop on Satellite Data Assimilation. 1. Overview. of NESDIS Contributions. to the JCSDA . Activities. Presented by. Sid Ahmed . Boukabara. Senior Data Assimilation Scientist, NESDIS/STAR. 1. Potential . OSSE for . Space. -based . Lidar. winds. . Michiko . Masutani . . A Nature Run (NR, proxy true atmosphere) is produced from a free forecast run using the highest resolution operational model which is significantly different from the NWP model used in Data Assimilation Systems.. GXS 101. . Dec. , 2022. Tim Schmit, NOAA NESDIS STAR . CoRP. ASPB. And many, many others ……. 1956. 1959. 1969. 1978. 1980. 1994. 1998. 2002. 2002. King: concept. Kaplan, sounding retrieval method. Privé. 22 November 2021. What is an Observing System . Simulation Experiment?. . A long free model run is used as the “truth” - the Nature Run. The Nature Run fields are used to back out “synthetic observations” from all current and new observing systems.