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contributor authorHARAGUCHI, PAUL Y.
date accessioned2017-06-09T15:58:39Z
date available2017-06-09T15:58:39Z
date copyright1968/03/01
date issued1968
identifier issn0027-0644
identifier otherams-57946.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4198338
description abstractTwo definite levels of subsidence inversions were found over the tropical Eastern Pacific Ocean during the winter of 1964; both were mainly persistent and continuous. The existence of the lower inversion has been known, but that of the upper inversion at a mean height of 550 mb. has not. It is hypothesized that the upper inversion is caused and maintained by the subsidence in the warm ?dynamic? anticyclone centered over Central America during winter. Both inversions appear to act as ?lids? on cloud height development.
publisherAmerican Meteorological Society
titleINVERSIONS OVER THE TROPICAL EASTERN PACIFIC OCEAN
typeJournal Paper
journal volume96
journal issue3
journal titleMonthly Weather Review
identifier doi10.1175/1520-0493(1968)096<0177:IOTTEP>2.0.CO;2
journal fristpage177
journal lastpage185
treeMonthly Weather Review:;1968:;volume( 096 ):;issue: 003
contenttypeFulltext


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