Asymmetric Frontal Response across the Gulf of Mexico Front in Winter 2016

Asymmetric Frontal Response across the Gulf of Mexico Front in Winter 2016

The interaction of cold-vertically stratified (CVS) Mississippi River water with warm-horizontally stratified (WHS) Gulf of Mexico water resulted in a front that affected the oceanic surface layer. Our cross-frontal observations demonstrated two vertical layers. The cross-frontal deep layer (9–30 m)...

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Bibliographic Details
Main Authors: Mohammad Barzegar, Darek Bogucki, Brian K. Haus, Tamay Ozgokmen, Mingming Shao
Format: Article
Language:English
Published: MDPI AG 2021-04-01
Series:Journal of Marine Science and Engineering
Subjects:
front
turbulence
heat flux
gulf of mexico
Online Access:https://www.mdpi.com/2077-1312/9/4/402

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