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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...
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| Опубликовано в: : | Sci Adv |
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| Главные авторы: | , |
| Формат: | Artigo |
| Язык: | Inglês |
| Опубликовано: |
American Association for the Advancement of Science
2018
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| Предметы: | |
| Online-ссылка: | 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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