Deep ocean currents detected with satellite altimetry
Overflows of dense and cold bottom water through Denmark Strait and the Faroe Bank Channel are associated with enhanced meso-scale current variability associated with eddies. These fluctuations can be detected through enhanced sea surface height variability in TOPEX/POSEIDON and ERS 1+2 satellite al...
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Format: | Text |
Language: | English |
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Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.534.9508 http://www.ifm.zmaw.de/fileadmin/files/images/Staff/Quadfasel/11cjrs_hoyer.pdf |