Composites of Heavy Rain Producing Elevated Thunderstorms in the Central United States

被引:3
|
作者
McCoy, Laurel P. [1 ]
Market, Patrick S. [1 ]
Gravelle, Chadm M. [2 ]
Graves, Charles E. [3 ]
Fox, Neil I. [1 ]
Rochette, Scott M. [4 ]
Kastman, Joshua [1 ]
Svoma, Bohumil [1 ]
机构
[1] Univ Missouri, Dept Soil Environm & Atmospher Sci, 302 ABNR, Columbia, MO 65211 USA
[2] Univ Wisconsin Madison, NOAA, NWS Training Ctr, NWS Operat Proving Ground,CIMSS SSEC, 7220 NW 101st Terr, Kansas City, MO 64153 USA
[3] St Louis Univ, Dept Earth & Atmospher Sci, ONeil Hall,Room 205A,3642 Lindell Blvd, St Louis, MO 63108 USA
[4] SUNY Coll Brockport, Coll Brockport, 350 New Campus Dr, Brockport, NY 14420 USA
基金
美国国家科学基金会;
关键词
FRONTAL SURFACES; POSITIVE CAPE; ENVIRONMENTS; STORMS;
D O I
10.1155/2017/6932798
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Composite analyses of the atmosphere over the central United States during elevated thunderstorms producing heavy rainfall are presented. Composites were created for five National Weather Service County Warning Areas (CWAs) in the region. Events studied occurred during the warm season (April-September) during 1979-2012. These CWAs encompass the region determined previously to experience the greatest frequency of elevated thunderstorms in the United States. Composited events produced rainfall of > 50mm 24 hr(-1) within the selected CWA. Composites were generated for the 0-3 hr period prior to the heaviest rainfall, 6-9 hours prior to it, and 12-15 hours prior to it. This paper focuses on the Pleasant Hill, Missouri (EAX) composites, as all CWA results were similar; also these analyses focus on the period 0-3 hours prior to event occurrence. These findings corroborate the findings of previous authors. What is offered here that is unique is (1) a measure of the interquartile range within the composite mean fields, allowing for discrimination between variable fields that provided a strong reliable signal, from those that may appear strong but possess large variability, and (2) composite soundings of two subclasses of elevated thunderstorms. Also, a null case (one that fits the composite but failed to produce significant rainfall) is also examined for comparison.
引用
收藏
页数:19
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