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06,  · SCIENCE DATA ANALYSIS Aerosol properties: Studies to characterize Polarization profiles from e CALIPSO lidar provide range-resolved identification of cloud ice/water phase, including e identification and characterization of optically in mixed phase clouds. CALIPSO observations toge er wi observations from CloudSat and o er A-train. science team. Some of ese activities are contributed as partnerships wi e project. including studies of e atmosphere, oceans, land surface, polar ice regions and solid Ear. e CloudSat mission will provide e first global survey of cloud properties at are critical for understanding eir effects on bo wea er and climate File Size: 1MB. Images/animation above: CloudSat science animation: CloudSat flies a first-of-its-kind radar system at is much more sensitive an any current wea er radar.CloudSat will provide new information about e vertical structure of clouds, including e quantities of liquid water and ice ey contain, and how clouds affect e distribution of e sun’s energy in e atmosphere. is event is a unique opportunity for e science community to strenghen eir cooperation in areas of research, data retrieval techniques and validation-verification activities. e workshop also serves e annual CloudSat-CALIPSO joint science team meeting. e workshop is open to scientists working wi in science areas. CloudSat and CALIPSO will provide a new, 3-D perspective on Ear 's clouds and air-borne particles called aerosols. e satellites will answer questions about how clouds and aerosols form, evolve and affect water supply, climate, wea er and air quality. CloudSat and CALIPSO employ revolutionary tools at will probe Ear 's atmosphere. CloudSat/CALIPSO Science Workshop. 28-31 y 2009. Monona Terrace, Madison WI. Abstracts of Oral Presentations. - A status report on e Science Team Recompetition - A status report on e ACE adal Survey Mission e ice scheme called SHIPS is unique in at ice particle properties (such as size, particle density 2009 Joint CALIPSO-CloudSat Science Team Meeting Held on y 28-31, 2009 e CALIPSO/CloudSat team meeting provided an opportunity for members of bo teams to discuss e data generated from CloudSat and CALIPSO and e future of e programs. In particular, e meeting focused on scientific discoveries and model improvements enabled by CloudSat and/or CALIPSO . CloudSat is currently in standby mode due to a spacecraft momentum wheel anomaly. Due to safety concerns, e CloudSat spacecraft will be executing a maneuver to lower it’s orbit and leave e A-Train. If at maneuver is successful, CloudSat should return to daytime-only operation sometime in e mid-February timeframe. CloudSat Standard Data Products. CloudSat Standard Data Products are distributed by e CloudSat Data Processing Center, located at e Cooperative Institute for Research in e Atmosphere at Colorado State University in Fort Collins.. Process Description/Interface Control Documents for e Standard Data Products be obtained here (CloudSat DPC site). Save e Date! CloudSat and CALIPSO Science Team Meeting ember 3–5, Greater Washington DC Area. e joint CALIPSO/CloudSat Science Team Meeting is a forum provided to e science team members to report on eir investigation activities to NASA management and to o er members of e CALIPSO and CloudSat science teams. CloudSat–CALIPSO Science Team Meeting. 01, . gave ree consecutive presentations on A New Estimate of e Influence of Clouds on Mass Balance of e Greenland Ice Sheet,, Relationships between Snow, Super-cooled Water, and Surface Radiation in e Arctic, and Assessing e Radiative Effects of Mixed-phase Clouds Using. At a meeting of e CloudSat and CALIPSO science teams to determine whe er CALIPSO should join its sister, ere was no debate. - One of e most re kable achievements by e CloudSat science team is e development of precipitation profile products. (light pink and dark red areas indicate e largest amount of ice/water). e. 4/29/ CERES Science Team Meeting 3 •Vertical distributions of LWC, IWC, and liquid and ice effective radii, are inputted from CloudSat's 2B-CWC Product •Temperature and relative humidity profiles from ECMWF •Surface albedo and emissivity from e International Geosphere-Biosphere Programme (IGBP) •Inputted into e Radiative transfer. At a meeting of e CloudSat and CALIPSO science teams to determine whe er CALIPSO should join its sister, ere was no debate. Literally no one came ford and said, 'I have an absolute burning need for CALIPSO to stay in e A-train,' said Charles Webb, who oversees NASA's fleet of operating Ear -orbiting satellites. e images above show some of e first images collected by active remote sensors on e CloudSat (top) and CALIPSO (lower) satellites at NASA launched in spring 2006. e top image is a vertical cross-section of Tropical Storm Alberto, e first named storm of e 2006 Atlantic Hurricane season, captured by a radar on CloudSat on e 12, 2006. AIRS Science Team Meeting, Pasadena, CA 27 ch 2007. 2 National Aeronautics and Space Administration CloudSat/Calypso. •Cloud liquid quantities from AMSR-E, MODIS and CloudSat. •Cloud ice quantities from MLS, CloudSat and AMSU-B on NOAA 16. CloudSat is a satellite mission designed to measure e vertical structure of clouds from space. e radar data produces detailed images of cloud structures. CloudSat is one of a constellation of satellites known as e A-Train (Cloudsat, CALIPSO, PARASOL, Aqua, Aura, GCOM-W1). e satellites fly in a nearly circular orbit wi an equatorial altitude of approximately 705 km. CloudSat will provide e first global survey of cloud properties at are crit-ical for understanding eir effects on bo wea er and climate. e key observations are vertical profiles of cloud liquid water and ice water. ese cloud properties are not obtainable from current satellite measurement systems. e mission's pri y science goal. Ear Science Reference Handbook [ Missions: CloudSat ] 125 CloudSat Sum y CloudSat will study clouds in detail to better characterize e role ey play in regulating Ear ’s climate. CloudSat will provide e first direct, global survey of e vertical structure and overlap of cloud systems and eir liquid- and ice-water contents. Troposphere Observed by AIRS, CloudSat, and CALIPSO: Quantifying Inter-hemispheric Humidity Differences Brian H. Kahn1, Andrew Gettelman2, Eric J. Fetzer1, Ann ie Eldering1, and Calvin K. Liang 3.. Jet Propulsion Laboratory, Caltech. 2. NCAR. 3. UCLA Department of Atmospheric and Oceanic Sciences. AIRS Science Team Meeting. e CloudSat/CALIPSO Science Team Meeting website has moved to of e highlights of each science team meeting is e competition between e scientists and e engineers for e honor of winning e CloudSat Cup. Past sporting events have included volleyball, hockey, bowling, and check-ers (yes, checkers!)—spanning e wide world of sports. Last year at e combined CloudSat/CALIPSO meeting. CloudSat, a NASA Ear System Science Pa finder Mission, will launch into orbit e world's most advanced wea er radar designed to measure properties of clouds at are essential for accurate understanding of Ear 's wea er and climate processes. Providing e first vertical profiles of global measurements of cloud ickness, height, water and ice content and a wide range of precipitation. Ice water content (IWC) profiles are derived from retrievals of optical extinction from e Cloud-Aerosol Lidar wi Or ogonal Polarization (CALIOP) satellite lidar, using a parameterization derived from particle probe measurements acquired during several aircraft field campaigns. Nadine Borduas, Neil M. Donahue, in Green Chemistry, . Ice Clouds. Ice clouds, also called cirrus clouds, are made up of ice crystals and start to form at altitudes of 5.5 km in temperate regions and of 6.5 km in tropical regions, making em e highest clouds in e troposphere. A small seed particle, or INP, is needed for heterogeneous ice nucleation. CloudSat Feature 2: Improving Climate Prediction Accuracy Who is on e CloudSat Science Team? Cloud Glossary Science Writer’s Guide to GRACE Q&A on GRACE e GRACE Instrument GRACE Feature 1: Tracking Water Movement on and Benea Ear ’s Surface GRACE Feature 2: Tracking Changes in Ice Sheets and Global Sea Level. e CloudSat DPC has released, to e CloudSat Science Team, a reprocessed R04 version of e 2B-GEOPROF-LIDAR product. is is e version at has been modified to account for e off-nadir pointing of CALIPSO and e CALIPSO VFM Version 2 reprocessing. e new files are identified as P1_R04 (e previous version was P_R04). Examining Cloud Changes over e Eastern Pacific Using CALIPSO and CloudSat 32ndCERES Science Team Meeting , 29–31, Lawrence Berkeley National Laboratory, Berkeley, CA, USA Seung-Hee Ham1, Seiji Kato2, Fred Rose1, Kuan-Man Xu2, and Tyler orsen2 1Science Systems and Applications, Inc. (SSAI), Hampton, Virginia, USA 2NASA Langley Research Center, Hampton, Virginia, USA. Evaluation of CERES-MODIS Cloud Properties Using CALIPSO and 31.. posted by vefa in 160. A comparison between CloudSat and aircraft data for. A complete understanding of e Ear ’s hydrologic cycle necessarily dictates an ability to accurately quantify e global range of precipitation rates and types (rain, snow etc.). In turn, global observations of precipitation are most efficiently made from space. Great strides in e measurement of global tropical rainfall have occurred recently as a result of e NASA Tropical Rainfall. Oreopoulos, L. Cho, N. Lee, D (). New insights about cloud vertical structure from CloudSat and CALIPSO observations. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 122(17), 9280-9300. Abstract Active cloud observations from A-Train's CloudSat and CALIPSO satellites offer new opportunities to examine e vertical structure of hydrometeor layers. 02 V 30 2 editor's corner In is Issue Ocean Surface Topography Science Team Meeting 23 Editor’s Corner Front Cover NASA High Mountain Asia Team Precipitation Workshop Sum y 27 Mission Status Report CloudSat Exits e A-Train 4 In e News Feature Articles NASA’s Longest Running Survey of Ice Shattered Records in 31. e official website for NASA Precipitation Measurement Missions. ese missions study rainfall and o er types precipitation around e globe. e Global Precipitation Measurement (GPM) mission provides a new generation of satellite observations of rain and snow worldwide every ree hours for scientific research and societal benefits. e GPM Core Observatory launched on February 27, . CloudSat will provide e first global observations of clouds using a satellite-based radar, revealing ickness, height, water and ice content, and a wide range of precipitation data. e CALIPSO satellite will provide vertical, curtain-like images of e atmosphere on a global scale using a lidar. 12, 2007 · In one study, a team led by Jennifer Kay at e National Center for Atmospheric Research, Boulder, Colo., examined e influence of polar clouds on 2007's record low extent of Arctic sea ice. Using data from CloudSat and NASA's Cloud-Aerosol Lidar and Infrared Pa finder Satellite Observation satellite, ey found e total cloud cover over e. Poster, CALIPSO CloudSat Science Team Meeting, Newport News, VG Assessing e radiative effects of global ice clouds based on CloudSat and CALIPSO measurements, 03/. Poster, AGU meeting Title: PhD in Atmospheric Science. Cloud Occurrence, Cloud Overlap, and Cloud Microphysics from e First Year of CloudSat and CALIPSO Data, Invited Presenation at e SORCE Science Team Meeting, February, 2008. Invited Talk/Keynote, Presented, 02/2008. Publications. Home Relationships between Ice Water Content and Volume Extinction Coefficient from Relationships between Ice Water Content and Volume Extinction Coefficient from e core information for is publication's citation. ADEOS Aqua Aquarius Aura CALIPSO CloudSat EO-1 GOES 13-15 GRACE ICESat Jason-1 Landsat 7 Landsat 8 OSTM/Jason-2 QuikSCAT Seasat 1 Sum y of e Ocean Surface Topography Science Team Meeting 13. NASA’s ICESat-2 Measures Arctic Ocean’s Sea Ice ickness, Snow Cover 26. NASA Space Laser Missions Map 16 Years of Ice Sheet Loss 28. TC4 Science Team Meeting CSC, Greenbelt MD 26 April 2007 TC4 Aqua (Terra) Validation, Science, and Enhance understanding of e global water cycle (vapor, clouds, snow/ice, soil ~200 km to e west to match CloudSat/CALIPSO when feasible). e CALIPSO lidar, also known as Cloud-Aerosol Lidar wi Or ogonal Polarization (CALIOP), complements CloudSat radar measurements by observing ice cloud particles at e top of Typhoon Yutu, which are too weak to be seen by e radar.CALIOP data is visualized above as a bluish cross-section, wi CPR data superimposed on it. CALIOP measured e top of e typhoon and its accompanying . Berry, E., G. Mace. Gettelman (), Using A-Train Observations to Evaluate East Pacific Cloud Occurrence and Radiative Effects in e Community Atmosphere Model, CloudSat/CALIPSO Science Team Meeting, Boulder, CO., . 3-5. Meeting Sum y 22 Darrel Williams Receives Pecora Sum y of e Twentie OMI Science Individual Ad 28 Team Meeting 26 OCO-2 Level-2, Build 8 Data Now CERES Science Team Meeting Sum y 29 Publicly Available 49 Sum y of e LANCE User Working Group Meeting 34 Regular Features Sum y of e LCLUC-SARI. STAR JPSS Annual Science Team Meeting, College Park, MD, .. Introduction. TIROS-1 (1960) [Rao. et al. (1990)] height definition for ice clouds is similar, except e average ice water Matching VIIRS wi CloudSat Match-up locations t. . CloudSat. 1353 UTC on 26 t . STAR JPSS Annual Science Team Meeting. • Suomi-NPP and CloudSat are in e same orbital plane, but at different altitudes • CloudSat and VIIRS overlap for ~4.5 hours every 2-3 days (8-9 matchups per mon) CBH for ice clouds is similar (T -dependent IWC). A research team at used NASA's QuikScat satellite to measure e extent and distribution of perennial and seasonal sea ice in e Arctic discovered at, while e total area of all e Arctic sea ice was stable in winter, e distribution of seasonal and perennial sea ice experienced significant changes. Kummerow, C., W. Berg, T. L'Ecuyer and S. C. van den Heever, 2009: Investigation of e role of aerosols and environmental conditions on precipitation onset in m clouds. e 19 Annual ARM Science Team Meeting, ch 30 April 3, 2009, Louisville, KY. 2009: 21.

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