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contributor authorDE VEAUX, EUGENE J.
date accessioned2017-06-09T15:55:34Z
date available2017-06-09T15:55:34Z
date copyright1955/10/01
date issued1955
identifier issn0027-0644
identifier otherams-56814.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4197081
description abstractThe height of the level of the sea at any time, exclusive of the astronomical tide, is closely related to the atmospheric pressure and the prevailing wind. Where the gaging station is situated on a tidal river the precipitation over the drainage basin may also be an influence. Important secular trends of these three elements are noted during the history of the tide gage at Charleston, S. C. The progressive rise in sea level as indicated by this gage may have been influenced by these trends.
publisherAmerican Meteorological Society
titleMETEOROLOGICAL TREND AND THE APPARENT RISE IN SEA LEVEL ALONG THE SOUTH CAROLINA COAST
typeJournal Paper
journal volume83
journal issue10
journal titleMonthly Weather Review
identifier doi10.1175/1520-0493(1955)083<0217:MTATAR>2.0.CO;2
journal fristpage217
journal lastpage224
treeMonthly Weather Review:;1955:;volume( 083 ):;issue: 010
contenttypeFulltext


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