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...
Những tác giả chính: | Buckingham, C, Garabato, A, Thompson, A, Brannigan, L, Lazar, A, Marshall, D, Nurser, A, Damerell, G, Heywood, K, Belcher, SE |
---|---|
Định dạng: | Journal article |
Được phát hành: |
AGU Publications
2016
|
Những quyển sách tương tự
-
Submesoscale instabilities in mesoscale eddies
Bằng: Brannigan, L, et al.
Được phát hành: (2017) -
The Contribution of Surface and Submesoscale Processes to Turbulence in the Open Ocean Surface Boundary Layer
Bằng: Christian E. Buckingham, et al.
Được phát hành: (2019-12-01) -
Submesoscale dynamics in the open ocean
Bằng: Brannigan, L
Được phát hành: (2015) -
Submesoscales are a significant turbulence source in global ocean surface boundary layer
Bằng: Jihai Dong, et al.
Được phát hành: (2024-11-01) -
The annual cycle of upper-ocean potential vorticity and its relationship to submesoscale instabilities
Bằng: Yu, X, et al.
Được phát hành: (2021)