The Mean Upper-Layer Flow in the Central Gulf of Mexico by a New Method
Previous studies have found a puzzling disagreement between two large datasets and the results of numerical models in the central Gulf of Mexico. The observations suggest an upper-layer mean flow to the west of order 10 cm s −1 , while the numerical models find no such mean flow. A new technique is...
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Veröffentlicht in: | Journal of physical oceanography 2016-10, Vol.46 (10), p.2915-2924 |
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description | Previous studies have found a puzzling disagreement between two large datasets and the results of numerical models in the central Gulf of Mexico. The observations suggest an upper-layer mean flow to the west of order 10 cm s
−1
, while the numerical models find no such mean flow. A new technique is used here, using 23 yr of satellite-derived sea surface height data, to estimate the mean flow. This third, independent set of data yields the same westward flow found in previous studies. These findings require that there be sinking in the western Gulf. The details of the return flow remain an intriguing problem. |
doi_str_mv | 10.1175/JPO-D-16-0062.1 |
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−1
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−1
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−1
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source | American Meteorological Society; EZB-FREE-00999 freely available EZB journals |
subjects | Flow Mathematical models Numerical models Return flow Sea surface Standard deviation Studies Wind |
title | The Mean Upper-Layer Flow in the Central Gulf of Mexico by a New Method |
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