PPT-Evaluation of convective precipitation using space-borne radar observation

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Kengo Matsubayashi Japan Meteorological Agency The Met Office Outline Motivation Observation and evaluation method Evaluation result Summary In many convection

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Evaluation of convective precipitation using space-borne radar observation: Transcript


Kengo Matsubayashi Japan Meteorological Agency The Met Office Outline Motivation Observation and evaluation method Evaluation result Summary In many convection schemes water substances are empirically modelled. Crystal K Williams. Department of Geography-Geology. Illinois State University. Outline. Introduction/Background. Mesoscale Convective Systems. Squall Lines. Precipitation. Conclusions. Introduction. 30. th. AMS Conference on Hurricanes and Tropical Meteorology. Matthew A. Janiga and Chris D. Thorncroft. University at Albany, SUNY. Niamey. Bamako. 500 km. Adapted from Fink and Reiner (2003). Squall Line Generation. . E. CHAM5-HAM. B. Croft. 1. , J.R. . . Pierce. 1. , R.V. Martin. 1,2. , C. Hoose. 3. , and U. Lohmann. 4. 1. Dalhouse University, Canada. 2. Harvard-Smithsonian Centre for Astrophysics, USA. 3. Karlsruhe Institute of Technology, Germany. . Juanzhen. . Sun. NCAR. , Boulder, . Colorado. Oct 25, . 2011. Outline. Introduction. . - Unique aspects of convective-scale DA. - Overview of techniques. Success and Issues. Future challenges. ACE is presently in pre-formulation and will be realized in some form in the early to mid . ’. 20s. . ACE is a response to the . The extreme sensitivity of the climate system to hydrological processes especially clouds and precipitation. Robert A. Houze, Jr.. University of Washington. with: K. L. Rasmussen, M. D. Zuluaga, and S. R. Brodzik. European Geosciences Union General Assembly, Vienna, Austria 17 April 2015 . The TRMM Satellite. Present and Near Future. Daniel S. . Berkowitz. Applications Branch. NWS . Radar Operations . Center. Norman. , . Oklahoma. 1. Paradigms of the . Past. One R(Z) relationship (a.k.a. Z-R or Z/R) could be used for the entire coverage (currently a 230 km range). o. bservations of mid-latitude . s. torms . d. uring OLYMPEX. Jennifer DeHart and Robert . Houze. 17. th. Conference on Mountain Meteorology. 6.28.16. NASA grants: NNX15AN52H, NNX13AG71G, NNX15AL38G, NNX16AD75G. Robert A. Houze, Jr.. University of Washington. with: K. L. Rasmussen, M. D. Zuluaga, and S. R. Brodzik. Presented at:. AGU Fall Meeting, San Francisco, 18 December 2015 . The TRMM Satellite. 1997-2014. Robert A. Houze, Jr.. With contributions from:. S. Powell, M. . Zuluaga. , H. Barnes, A. Rowe. AGU Annual Meeting, San Francisco, 11 December 2013. The MJO scale. ~30-60 days. TOGA. COARE. West Pacific. ?. Himalayas. Andes. Rockies. New Fellows Presentation, . AGU, San Francisco, . 5 . December 2012. Robert A. Houze, Jr.. University of Washington. Radars in Space. TRMM. 1997-. CloudSat. 2006-. Typical Tropical Convective Cloud Population. , Jr.. University of Washington. 2015 US-Taiwan Extreme Precipitation and Weather Workshop. Taipei, Taiwan. 29 May 2015. Microphysical characteristics of orographic precipitation: Insights from TiMREX and beyond. Bryce Harrop. Postdoc RA. Pacific Northwest National Laboratory. (509) 375-2696. bryce.harrop@pnnl.gov. climatemodeling.science.energy.gov/acme. The Role of Convective Gustiness in Reducing Seasonal Precipitation Biases in the Tropical West . Precipitation mechanisms. Rainall. maps. Rainfall hyetographs. Nexrad. measurement of rainfall. Reading: Applied Hydrology Sections . 3.5 . to . 3.6 . on . Evaporation for Thursday. Precipitation. Precipitation: water falling from the atmosphere to the earth..

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