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contributor authorMcNulty, Richard P.
date accessioned2017-06-09T14:44:56Z
date available2017-06-09T14:44:56Z
date copyright1991/03/01
date issued1991
identifier issn0882-8156
identifier otherams-2588.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4162711
description abstractA microburst occurred at Goodland, Kansas, on 4 March 1990. This event was unique in the sense that it occurred at 0348 AM MST (1048 UTC) and produced 14°F (7.8°C) of warming. The environment along the High Plains exhibited characteristics similar to those associated with dry microbursts documented in the literature. Examination of an interpolated sounding for Goodland implied that evaporational cooling would need to occur throughout most of the dry sub-cloud layer to support the observed surface temperature.
publisherAmerican Meteorological Society
titleDownbursts from Innocuous Clouds: An Example
typeJournal Paper
journal volume6
journal issue1
journal titleWeather and Forecasting
identifier doi10.1175/1520-0434(1991)006<0148:DFICAE>2.0.CO;2
journal fristpage148
journal lastpage154
treeWeather and Forecasting:;1991:;volume( 006 ):;issue: 001
contenttypeFulltext


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