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dc.contributor.authorMori, Yukihiro
dc.date.accessioned2017-06-09T15:06:52Z
dc.date.available2017-06-09T15:06:52Z
dc.date.copyright1988/02/01
dc.date.issued1988
dc.identifier.issn0894-8755
dc.identifier.otherams-3472.pdf
dc.identifier.urihttp://onlinelibrary.yabesh.ir/handle/yetl/4172534
dc.description.abstractUsing the winds in Japan as an example, the validity of the vectorial treatment of the surface wind in climatological investigations has been demonstrated, and the expressions for climatological mean and variability of the wind have been reviewed. The annual resultant surface winds tend to be westerly at latitudes higher than 30° and easterly at lower latitudes. At lower latitudes, the mean surface winds and the mean 850 mb winds are almost opposite to each other in direction at times. Climatological mean wind directions according to different definitions have been investigated for the surface wind. The means of wind direction agree with the directions of the vector mean wind within 30° where the magnitudes of the vector mean wind are larger than 1.5 m s?1. The relationships between the two measures of the constancy of the wind are investigated.
dc.publisherAmerican Meteorological Society
dc.titleA Study on Climatological Aspects of Winds in Japan. Part I: Mean Wind Fields and Annual Variations of Winds
dc.typeJournal Paper
dc.journal.volume1
dc.journal.issue2
dc.journal.titleJournal of Climate
dc.identifier.doi10.1175/1520-0442(1988)001<0132:ASOCAO>2.0.CO;2
dc.journal.fristpage132
dc.journal.lastpage142
dc.treeJournal of Climate:;1988:;volume( 001 ):;issue: 002
dc.contenttypeFulltext


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