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contributor authorRiehl, Herbert
contributor authorShafer, Robert J.
date accessioned2017-06-09T14:09:35Z
date available2017-06-09T14:09:35Z
date copyright1944/09/01
date issued1944
identifier issn0095-9634
identifier otherams-13518.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4148977
description abstractThe relations between major alterations of the paths of tropical storms and the upper windfield, especially changes in the height of the base of the polar westerlies, are examined in detail. If the base lowers greatly west of a storm in connection with an eastward moving middle-latitude trough, and remains low, northward recurvature will take place. If the upper westerlies cannot maintain themselves in low latitudes; however, the storm will bypass the northern trough and continue to travel westward. Similar riles are stated for several types of abnormal hurricane tracks, and some observations are made on the formation of tropical storms.
publisherAmerican Meteorological Society
titleTHE RECURVATURE OF TROPICAL STORMS
typeJournal Paper
journal volume1
journal issue1
journal titleJournal of Meteorology
identifier doi10.1175/1520-0469(1944)001<0001:TROTS>2.0.CO;2
journal fristpage42
journal lastpage54
treeJournal of Meteorology:;1944:;volume( 001 ):;issue: 001
contenttypeFulltext


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