A COMPARISON OF DIRECT OBSERVATIONS OF VELOCITY AND TRANSPORT IN THE WINDWARD PASSAGE

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dc.contributor.author Bulgakov S.N.
dc.contributor.author Bulgakov N.P.
dc.contributor.author Ivanov V.A.
dc.date.accessioned 2022-02-07T05:09:35Z
dc.date.available 2022-02-07T05:09:35Z
dc.date.issued 2003
dc.identifier https://elibrary.ru/item.asp?id=27769186
dc.identifier.citation Geofisica International, 2003, 42, 1, 115-129
dc.identifier.issn 0016-7169
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/35064
dc.description.abstract Velocity and water transport through the Windward Passage is estimated from a review of prior investigations and a new analysis of mooring observations conducted on February, 18, 1965 and November, 19-23, 1970 in the former USSR. These may be the only available direct velocity measurements in this area. Direct current measurements indicate a transport of about 8 Sv ± 4 Sv into the Caribbean sea, which is consistent with values estimated by other authors. The transport figure based on November, 19- 23, 1970 data is interpreted as a surface outflow of 0.8 Sv in the upper 100 m, a mid-depth inflow of 10.7 Sv in the 100-700 m layer, and an outflow of 2.0 Sv below 700 m. The general current-countercurrent flow system of the upper 200 m in Windward Passage compares satisfactorily with recent ADCP observations in the Great Inagua Passage.
dc.subject Windward Passage
dc.subject current measurements
dc.subject data comparison
dc.title A COMPARISON OF DIRECT OBSERVATIONS OF VELOCITY AND TRANSPORT IN THE WINDWARD PASSAGE
dc.type Статья


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