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contributor authorMalardé, Jean-Pierre
contributor authorPerigaud, Claire
contributor authorDe Mey, Pierre
contributor authorMinster, Jean-Francois
date accessioned2017-06-09T14:48:41Z
date available2017-06-09T14:48:41Z
date copyright1987/12/01
date issued1987
identifier issn0022-3670
identifier otherams-27295.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4164284
description abstractSynoptic maps of the mesoscale dynamic topography in a band between 7.5°N and 7.5°S in the Pacific Ocean are drawn from Seasat altimeter data. They show a set of eddies 600 km in diameter and 15?20 cm in amplitude moving westward with a velocity of about 40 km day?1 along 4.5°N. Their occurrence is consistent with the surface temperature front undulations observed by Legeckis. South of the equator the signal is less coherent, but a significant degree of symmetry with the north is evidenced. The dynamics of the wave system might also present some degree of nonlinearity, as some water seems to be carried along with the wave.
publisherAmerican Meteorological Society
titleObservation of Long Equatorial Waves in the Pacific Ocean by Seasat Altimetry
typeJournal Paper
journal volume17
journal issue12
journal titleJournal of Physical Oceanography
identifier doi10.1175/1520-0485(1987)017<2273:OOLEWI>2.0.CO;2
journal fristpage2273
journal lastpage2279
treeJournal of Physical Oceanography:;1987:;Volume( 017 ):;issue: 012
contenttypeFulltext


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