Seasonality of submesoscale flows in the ocean surface boundary layer

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...

Полное описание

Библиографические подробности
Главные авторы:	Buckingham, C, Garabato, A, Thompson, A, Brannigan, L, Lazar, A, Marshall, D, Nurser, A, Damerell, G, Heywood, K, Belcher, SE
Формат:	Journal article
Опубликовано:	AGU Publications 2016

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