PPT-Stratiform vs Convective

Ref Vel stratiform Convall radref Cloud analysis followed by 3dvar Convuv spd rw Only 3dvar analysis Applied DFI to Qv only other mosit variable like Qs Qc Qr Qg Qi are remain unchanged and. Hannah C. Barnes. Robert A. Houze, Jr.. University of Washington. 31. st. Conference on Hurricanes and Tropical Meteorology . Town & Country Resort and Conference Center, San Diego, CA. 2 April 2014. Hannah C. Barnes. Robert A. Houze, Jr.. University of Washington. Presentation by H. Barnes at Department of Meteorology, . The Pennsylvania . State University, State . Callege. , PA, August 15, 2014. Kristen . Lani. Rasmussen. Robert A. Houze, Jr. . ICAM 2013, . Kranjska. Gora, June 6th. Convective . “. h. ot spots. ”. occur near major mountain ranges (. Zipser. et al. 2006). Most Intense Thunderstorms on Earth. Brian Guyer & Deirdre Kann, National Weather Service, Albuquerque, NM. Project Summary. OBJECTIVE: . Test the growing suite of convective initiation products to determine their potential to improve forecasts and detection of hazardous convective events during the North American monsoon season.. . Insurance Trends and Challenges in an Era of Climate Volatility. National Tornado Summit. Oklahoma City, OK. February 11, 2014. Robert P. Hartwig, Ph.D., CPCU, President & Economist. Insurance Information Institute  110 William Street  New York, NY 10038. . Early Results from DYNAMO. Int. Conf. on Opportunities and Challenges in Monsoon Prediction in a Changing Climate. Golden Jubilee. . of the Indian Institute of Tropical Meteorology, Pune. , . India, 23 February, 2012. Challenges for the Next Decades. NASA Earth Science Division Workshop, NASA/Ames, 6-8 May 2014. Robert A. Houze, Jr.. University of Washington. Fair weather cumulus. Cumulus congestus. Cumulonimbus. Single cell. Bjerknes. Memorial Lecture, AGU, San Francisco, 4 December 2012. Robert Houze. University of Washington. A personal story of three great field campaigns and the evolution of meteorological satellites . Loosely defined: A line of either ordinary cells or supercells of finite length (10- hundreds of km) that may contain a stratiform rain region either behind, parallel to, or ahead of the convective line.. 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. 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. Courtney Schumacher for Brian’s mesoscale . class. First tropical radar bright band. Murty. et al. (1965). African squall line evolution. Chong et al. (1987). African squall line (mature stage). Chong et al. (1987). 2. from TOGA COARE*. Richard H. Johnson . Paul E. . Ciesielski. Colorado State University. Thomas M. . Rickenbach. East Carolina University. * . D. edicated to . Michio. . Yanai. (AMS Monograph). Yanai. R. Houze, K. . Virts. , A. K. Rowe, M. D. . Zuluaga. University of Washington. CloudSat Science Team Meeting, Alexandria, VA, 5 November 2014. —as seen by. A-Train and TRMM. Johnson & Houze 1987.