Determination of water mass properties of water pumped down from the Ekman layer to the geostrophic flow below
In a subtropical gyre, the convergent Ekman layer forces water downward into the geostrophic flow below. The properties and depth of the mixed layer vary considerably during the course of the year, but this variability does not penetrate into the geostrophic region. Evidently there is some process a...
Αποθηκεύτηκε σε:
| Εκδόθηκε σε: | Proc Natl Acad Sci U S A |
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| Κύριος συγγραφέας: | |
| Μορφή: | Artigo |
| Γλώσσα: | Inglês |
| Έκδοση: |
National Academy of Sciences
1979
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| Θέματα: | |
| Διαθέσιμο Online: | https://ncbi.nlm.nih.govhttps://pmc.ncbi.nlm.nih.gov/articles/PMC383760/ https://ncbi.nlm.nih.govhttps://pubmed.ncbi.nlm.nih.gov/16592670/ https://ncbi.nlm.nih.govhttps://doi.org/10.1073/pnas.76.7.3051 |
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