<--- Back to Details
| First Page | Document Content | |
|---|---|---|
 Date: 2010-08-04 15:53:24Atmospheric thermodynamics Wind Radar meteorology Microscale meteorology Bow echo Rear-inflow jet Atmospheric convection Bulk Richardson number Convective available potential energy Atmospheric sciences Meteorology Storm |
Add to Reading List |
950 MONTHLY WEATHER REVIEW VOLUME 134 | PDF DocumentDocID: 1prmw - View Document |
| Microsoft Word - PartC_NewAppendixB_Rev10.docDocID: 17KAP - View Document |
| Microsoft Word - PartD_AppendixB_Rev9.docDocID: 17CA2 - View Document |
| CHAPTER 7 MORPHOLOGY OF LARGE-SCALE PRECIPITATING WEATHER SYSTEMS 7.1 Introduction. The character of precipitation is largely controlled by vertical air motions, static stability, horizontal kinematics (e.g., deformatioDocID: 12vSl - View Document |
| Toward the Long-range Prediction of Severe Convective Windstorms Ken Pryor Department of Atmospheric and Oceanic Science, University of Maryland, College Park/NOAACenter for Satellite Applications and ResearchDocID: 11ngr - View Document |