Observation of long first-mode baroclinic Rossby waves in the North Atlantic and their connection with wind forcing
Residual sea surface height anomaly fields are obtained over the North Atlantic Basin from TOPEX/Poseidon altimeter data. Evidence of westward propagating anomalies characterized as first-mode baroclinic Rossby waves is presented. The sea surface height signal is divided into two spectral bands, the...
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Format: | Text |
Language: | English |
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DigitalCommons@URI
1997
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Online Access: | https://digitalcommons.uri.edu/dissertations/AAI9805246 |