contributor author | Weaver, John F. | |
contributor author | Toth, James J. | |
date accessioned | 2017-06-09T14:43:48Z | |
date available | 2017-06-09T14:43:48Z | |
date copyright | 1990/06/01 | |
date issued | 1990 | |
identifier issn | 0882-8156 | |
identifier other | ams-2541.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4162190 | |
description abstract | Conditions leading up to an outbreak of severe hailstorms in northeast Colorado are examined using satellite and surface data. A persistent mesoscale ridge of surface-high pressure, caused by outflow from a mesoscale- convective system, is seen to coincide with the occurrence of large hail which was confined to a narrow band extending nearly parallel to the Front Range of the Rocky Mountains. The development of the mesoscale ridge during its most intense stages is documented using a procedure that yields an approximate streamfunction for the surface geostrophic wind. Unlike alternatives over sloping terrain, this method is quick and can be adjusted to minimize the error over a limited portion of the analysis area. | |
publisher | American Meteorological Society | |
title | The Use of Satellite Imagery and Surface Pressure-Gradient Analysis Modified for Sloping Terrain to Analyze the Mesoscale Events Preceding the Severe Hailstorms of 2 August 1986 | |
type | Journal Paper | |
journal volume | 5 | |
journal issue | 2 | |
journal title | Weather and Forecasting | |
identifier doi | 10.1175/1520-0434(1990)005<0279:TUOSIA>2.0.CO;2 | |
journal fristpage | 279 | |
journal lastpage | 298 | |
tree | Weather and Forecasting:;1990:;volume( 005 ):;issue: 002 | |
contenttype | Fulltext | |