Vertical Structure of Ocean Mesoscale Eddies with Implications for Parameterizations of Tracer Transport
Abstract The Gent–McWilliams parameterization is commonly used in global ocean models to model the advective component of tracer transport effected by unresolved mesoscale eddies. The vertical structure of the transfer coefficient in this parameterization is studied using data from a 0.1° resolution...
Main Authors: | Z. Stanley, S. D. Bachman, I. Grooms |
---|---|
Format: | Article |
Language: | English |
Published: |
American Geophysical Union (AGU)
2020-10-01
|
Series: | Journal of Advances in Modeling Earth Systems |
Subjects: | |
Online Access: | https://doi.org/10.1029/2020MS002151 |
Similar Items
-
A Diagnosis of Anisotropic Eddy Diffusion From a High‐Resolution Global Ocean Model
by: Scott D. Bachman, et al.
Published: (2020-02-01) -
Dimensões geopolíticas do modernismo. Contraculturas mexicanas na Califórnia
by: Maria José Canelo
Published: (2006-06-01) -
Comparing Two Parameterizations for the Restratification Effect of Mesoscale Eddies in an Isopycnal Ocean Model
by: Nora Loose, et al.
Published: (2023-12-01) -
Parameterizing Mesoscale Eddy Buoyancy Transport Over Sloping Topography
by: Aleksi Nummelin, et al.
Published: (2024-03-01) -
Toward an Energetically Consistent, Resolution Aware Parameterization of Ocean Mesoscale Eddies
by: Malte F. Jansen, et al.
Published: (2019-08-01)