Seasonality of submesoscale flows in the ocean surface boundary layer
A signature of submesoscale flows in the upper ocean is skewness in the distribution of relative vorticity. Expected to result for high Rossby number flows, such skewness has implications for mixing, dissipation, and stratification within the upper ocean. An array of moorings deployed in the Northea...
| Автори: | , , , , , , , , , |
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| Формат: | Journal article |
| Опубліковано: |
AGU Publications
2016
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