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contributor authorNoble, Marlene
contributor authorCacchione, David A.
contributor authorSchwab, William C.
date accessioned2017-06-09T14:48:58Z
date available2017-06-09T14:48:58Z
date copyright1988/09/01
date issued1988
identifier issn0022-3670
identifier otherams-27406.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4164408
description abstractLarge semidiurnal current and isotherm oscillations were observed by one current meter continuously for 9 months in the waters above Horizon Guyot, a seamount located in the central Pacific. The M2 tides dominated the current-meter record. The M2 current ellipse was oriented along 142°; the semi-major amplitude was 7.6 cm s?1 and the currents rotated in a clockwise direction. The M2 isotherm deflection amplitude was 20 m. The M2 currents observed above the guyot were two to three times larger than M2 currents either observed in or predicted for this region of the mid-Pacific. Evidence suggests that the semidiurnal tide was predominantly an internal tide that was generated at the guyot. The observed internal tide had a narrow bandwidth and a constant amplitude and phase for 9 months, and had characteristics similar to a vertically propagating, rather than a vertically standing, internal wave.
publisherAmerican Meteorological Society
titleObservations of Strong Mid-Pacific Internal Tides above Horizon Guyot
typeJournal Paper
journal volume18
journal issue9
journal titleJournal of Physical Oceanography
identifier doi10.1175/1520-0485(1988)018<1300:OOSMPI>2.0.CO;2
journal fristpage1300
journal lastpage1306
treeJournal of Physical Oceanography:;1988:;Volume( 018 ):;issue: 009
contenttypeFulltext


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