The Contribution of Surface and Submesoscale Processes to Turbulence in the Open Ocean Surface Boundary Layer-Reference-Cited by-同舟云学术

The Contribution of Surface and Submesoscale Processes to Turbulence in the Open Ocean Surface Boundary Layer

Published:2019-12 Issue:12 Volume:11 Page:4066-4094
ISSN:1942-2466
Container-title:Journal of Advances in Modeling Earth Systems
language:en
Short-container-title:J. Adv. Model. Earth Syst.

Author:

Buckingham Christian E.¹^ORCID,Lucas Natasha S.²^ORCID,Belcher Stephen E.³,Rippeth Tom P.²^ORCID,Grant Alan L. M.⁴,Le Sommer Julien⁵^ORCID,Ajayi Adekunle Opeoluwa⁵^ORCID,Naveira Garabato Alberto C.⁶^ORCID

Affiliation:

1. British Antarctic Survey Cambridge UK

2. School of Ocean SciencesBangor University Bangor UK

3. Met Office Exeter UK

4. Department of MeteorologyUniversity of Reading Reading UK

5. University of Grenoble Alpes/CNRS/IRD/G‐INP, IGE Grenoble France

6. Ocean and Earth ScienceUniversity of Southampton Southampton UK

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Environmental Chemistry,Global and Planetary Change

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2019MS001801

Reference100 articles.

1. Frontal Circulation and Submesoscale Variability during the Formation of a Southern Ocean Mesoscale Eddy

2. Near-Inertial Internal Gravity Waves in the Ocean

3. Effects of three-dimensionality on instability and turbulence in a frontal zone

4. Parameterization of Frontal Symmetric Instabilities. I: Theory for Resolved Fronts

5. A global perspective on Langmuir turbulence in the ocean surface boundary layer

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