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contributor authorVose, Russell S.
contributor authorApplequist, Scott
contributor authorBourassa, Mark A.
contributor authorPryor, Sara C.
contributor authorBarthelmie, Rebecca J.
contributor authorBlanton, Brian
contributor authorBromirski, Peter D.
contributor authorBrooks, Harold E.
contributor authorDeGaetano, Arthur T.
contributor authorDole, Randall M.
contributor authorEasterling, David R.
contributor authorJensen, Robert E.
contributor authorKarl, Thomas R.
contributor authorKatz, Richard W.
contributor authorKlink, Katherine
contributor authorKruk, Michael C.
contributor authorKunkel, Kenneth E.
contributor authorMacCracken, Michael C.
contributor authorPeterson, Thomas C.
contributor authorShein, Karsten
contributor authorThomas, Bridget R.
contributor authorWalsh, John E.
contributor authorWang, Xiaolan L.
contributor authorWehner, Michael F.
contributor authorWuebbles, Donald J.
contributor authorYoung, Robert S.
date accessioned2017-06-09T16:44:41Z
date available2017-06-09T16:44:41Z
date copyright2014/03/01
date issued2013
identifier issn0003-0007
identifier otherams-73335.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4215438
description abstractntific assessment examines changes in three climate extremes?extratropical storms, winds, and waves?with an emphasis on U.S. coastal regions during the cold season. There is moderate evidence of an increase in both extratropical storm frequency and intensity during the cold season in the Northern Hemisphere since 1950, with suggestive evidence of geographic shifts resulting in slight upward trends in offshore/coastal regions. There is also suggestive evidence of an increase in extreme winds (at least annually) over parts of the ocean since the early to mid-1980s, but the evidence over the U.S. land surface is inconclusive. Finally, there is moderate evidence of an increase in extreme waves in winter along the Pacific coast since the 1950s, but along other U.S. shorelines any tendencies are of modest magnitude compared with historical variability. The data for extratropical cyclones are considered to be of relatively high quality for trend detection, whereas the data for extreme winds and waves are judged to be of intermediate quality. In terms of physical causes leading to multidecadal changes, the level of understanding for both extratropical storms and extreme winds is considered to be relatively low, while that for extreme waves is judged to be intermediate. Since the ability to measure these changes with some confidence is relatively recent, understanding is expected to improve in the future for a variety of reasons, including increased periods of record and the development of ?climate reanalysis? projects.
publisherAmerican Meteorological Society
titleMonitoring and Understanding Changes in Extremes: Extratropical Storms, Winds, and Waves
typeJournal Paper
journal volume95
journal issue3
journal titleBulletin of the American Meteorological Society
identifier doi10.1175/BAMS-D-12-00162.1
journal fristpage377
journal lastpage386
treeBulletin of the American Meteorological Society:;2013:;volume( 095 ):;issue: 003
contenttypeFulltext


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