An Ocean Resonance in the Southeast Pacific
Satellite Altimeter observations of sea surface height show an extensive region of high variability in the Southeastern Pacific which previous studies have suggested is a Rossby wave trapped by topography. Here we investigate the feature using results from a high‐resolution global ocean model. We ca...
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Published in | Geophysical research letters Vol. 29; no. 8; pp. 93-1 - 93-3 |
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Main Authors | , |
Format | Journal Article |
Language | English |
Published |
American Geophysical Union
01.04.2002
Blackwell Publishing Ltd |
Subjects | |
Online Access | Get full text |
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Summary: | Satellite Altimeter observations of sea surface height show an extensive region of high variability in the Southeastern Pacific which previous studies have suggested is a Rossby wave trapped by topography. Here we investigate the feature using results from a high‐resolution global ocean model. We calculate the empirical orthogonal modes and find that 29% of the SSH variability is due to a single mode. We correlate the time series of the mode with the local Ekman pumping and find that the correlation is largest when the wind curl is averaged over a region roughly the size of the mode. We calculate the response function relating the two time series and find that it is dominated by a resonance at zero frequency with a decay time of about two days. We conclude that the feature is a highly damped geostrophic mode of the ocean. |
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Bibliography: | ArticleID:2001GL014259 istex:88F29EE33C2253A1A54F83CEC1C47723861EFA01 ark:/67375/WNG-N74KK3JT-7 ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 23 ObjectType-Article-2 ObjectType-Feature-1 |
ISSN: | 0094-8276 1944-8007 |
DOI: | 10.1029/2001GL014259 |