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contributor authorLyons, Steven W.
date accessioned2017-06-09T15:08:45Z
date available2017-06-09T15:08:45Z
date copyright1989/01/01
date issued1989
identifier issn0894-8755
identifier otherams-3563.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4173545
description abstractA zonal wind oscillation with a period of about 15?35 days is isolated over the middle latitudes of the Northern Hemisphere during winter. A systematic relationship between the zonal winds and wind departures from zonal symmetry (eddies) is found for nine prominent zonal wind oscillation cycles taken from six 120-day winters. This zonal/eddy relationship consists of an oscillation between anomalous zonal flow and anomalous meridional flow, which is strongest across North America from 150°W to 0°.
publisherAmerican Meteorological Society
titleAdditional Evidence of an Upper Tropospheric Zonal/Eddy Relationship during Winter
typeJournal Paper
journal volume2
journal issue1
journal titleJournal of Climate
identifier doi10.1175/1520-0442(1989)002<0091:AEOAUT>2.0.CO;2
journal fristpage91
journal lastpage100
treeJournal of Climate:;1989:;volume( 002 ):;issue: 001
contenttypeFulltext


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