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)...
| الحاوية / القاعدة: | Journal of Marine Science and Engineering |
|---|---|
| المؤلفون الرئيسيون: | , , , , |
| التنسيق: | مقال |
| اللغة: | الإنجليزية |
| منشور في: |
MDPI AG
2021-04-01
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| الموضوعات: | |
| الوصول للمادة أونلاين: | https://www.mdpi.com/2077-1312/9/4/402 |