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contributor authorClapp, Philip F.
contributor authorWinston, Jay S.
date accessioned2017-06-09T14:10:26Z
date available2017-06-09T14:10:26Z
date copyright1951/08/01
date issued1951
identifier issn0095-9634
identifier otherams-13848.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4149343
description abstractThis is the second report on a continuing project designed to investigate quantitatively the confluence process and associated changes in the strength and location of the mid-tropospheric jet stream. An empirical study has been made of a case of large-scale confluence as observed on a sequence of 5-day mean charts. It is found that the local change in wind speed is related to the relative advection of cold and warm air on either side of the jet axis and also to the advection of wind speed along the axis. Tentative estimates of vertical motion indicate sinking motion in the cold air north of the jet axis and rising motion in the warm air to the south.
publisherAmerican Meteorological Society
titleA CASE STUDY OF CONFLUENCE AS RELATED TO THE JET STREAM
typeJournal Paper
journal volume8
journal issue4
journal titleJournal of Meteorology
identifier doi10.1175/1520-0469(1951)008<0231:ACSOCA>2.0.CO;2
journal fristpage231
journal lastpage243
treeJournal of Meteorology:;1951:;volume( 008 ):;issue: 004
contenttypeFulltext


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