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contributor authorKunkel, Kenneth E.
contributor authorEasterling, David R.
contributor authorKristovich, David A. R.
contributor authorGleason, Byron
contributor authorStoecker, Leslie
contributor authorSmith, Rebecca
date accessioned2017-06-09T17:14:25Z
date available2017-06-09T17:14:25Z
date copyright2012/06/01
date issued2012
identifier issn1525-755X
identifier otherams-81669.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4224697
description abstractaily extreme precipitation events, exceeding a threshold for a 1-in-5-yr occurrence, were identified from a network of 935 Cooperative Observer stations for the period of 1908?2009. Each event was assigned a meteorological cause, categorized as extratropical cyclone near a front (FRT), extratropical cyclone near center of low (ETC), tropical cyclone (TC), mesoscale convective system (MCS), air mass (isolated) convection (AMC), North American monsoon (NAM), and upslope flow (USF). The percentage of events ascribed to each cause were 54% for FRT, 24% for ETC, 13% for TC, 5% for MCS, 3% for NAM, 1% for AMC, and 0.1% for USF. On a national scale, there are upward trends in events associated with fronts and tropical cyclones, but no trends for other meteorological causes. On a regional scale, statistically significant upward trends in the frontal category are found in five of the nine regions. For ETCs, there are statistically significant upward trends in the Northeast and east north central. For the NAM category, the trend in the West is upward. The central region has seen an upward trend in events caused by TCs.
publisherAmerican Meteorological Society
titleMeteorological Causes of the Secular Variations in Observed Extreme Precipitation Events for the Conterminous United States
typeJournal Paper
journal volume13
journal issue3
journal titleJournal of Hydrometeorology
identifier doi10.1175/JHM-D-11-0108.1
journal fristpage1131
journal lastpage1141
treeJournal of Hydrometeorology:;2012:;Volume( 013 ):;issue: 003
contenttypeFulltext


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