The lower branch of the thermohaline circulation in the Atlantic Ocean is driven by two sources: the convec-tion in the Labrador Sea (LS) and the overflows across the Greenland Scotland Ridge (GSR), which are fed
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| Format: | Text |
| Language: | English |
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| Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.608.7753 |
| Summary: | The lower branch of the thermohaline circulation in the Atlantic Ocean is driven by two sources: the convec-tion in the Labrador Sea (LS) and the overflows across the Greenland Scotland Ridge (GSR), which are fed |
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