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contributor authorPlatzman, George W.
contributor authorCurtis, Gary A.
contributor authorHansen, Kirk S.
contributor authorSlater, Richard D.
date accessioned2017-06-09T14:45:50Z
date available2017-06-09T14:45:50Z
date copyright1981/05/01
date issued1981
identifier issn0022-3670
identifier otherams-26221.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4163092
description abstractWe have calculated normal modes with period between 8 and 80 h for a domain consisting of the Arctic, Atlantic, Indian and Pacific oceans. In this period range the numerical model has 56 modes, of which 13 are topographic vorticity waves all slower than 30 h. The trapping sites for these modes are the Siberian Shelf, the Icelandic Plateau, the Grand Banks, the Falkland Plateau and Patagonian Shelf, the Kerguelen Plateau, the New Zealand and Fiji Plateaus, and the Hawaiian Ridge. Predominantly planetary vorticity waves do not appear in the model at periods less than 80 h. The 41 modes found between 30 and 8 h include basin modes in the North Atlantic, Indian and equatorial Pacific; quarter-wave resonances in the Arabian Sea, Bay of Bengal and Gulf of Guinea; and Kelvin waves on the Antarctic coast, the Pacific North American coast and the New Zealand coast. Several vorticity and gravity modes exhibit an eastward circumglobal flow of energy that is confined to equatorial latitudes except where deflected southward by the continental land masses of the Southern Hemisphere. Tide-gage data are cited as consistent with 25.8 and 14.1 h basin modes in the North Atlantic and with the three Kelvin waves noted above, whose periods are 28.7, 15.5 and 10.8 h, respectively.
publisherAmerican Meteorological Society
titleNormal Modes of the World Ocean. Part II: Description of Modes in the Period Range 8 to 80 Hours
typeJournal Paper
journal volume11
journal issue5
journal titleJournal of Physical Oceanography
identifier doi10.1175/1520-0485(1981)011<0579:NMOTWO>2.0.CO;2
journal fristpage579
journal lastpage603
treeJournal of Physical Oceanography:;1981:;Volume( 011 ):;issue: 005
contenttypeFulltext


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