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Submesoscale-selective compensation of fronts in a salinity-stratified ocean
Salinity, rather than temperature, is the leading influence on density in some regions of the world’s upper oceans. In the Bay of Bengal, heavy monsoonal rains and runoff generate strong salinity gradients that define density fronts and stratification in the upper ~50 m. Ship-based observations made...
Gorde:
| Argitaratua izan da: | Sci Adv |
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| Egile Nagusiak: | , |
| Formatua: | Artigo |
| Hizkuntza: | Inglês |
| Argitaratua: |
American Association for the Advancement of Science
2018
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| Gaiak: | |
| Sarrera elektronikoa: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5834007/ https://ncbi.nlm.nih.gov/pubmed/29507874 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1126/sciadv.1701504 |
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