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

dc.contributor.authorBulgakov S.N.
dc.contributor.authorBulgakov N.P.
dc.contributor.authorIvanov V.A.
dc.date.accessioned2022-02-07T05:09:35Z
dc.date.available2022-02-07T05:09:35Z
dc.date.issued2003
dc.description.abstractVelocity 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.identifierhttps://elibrary.ru/item.asp?id=27769186
dc.identifier.citationGeofisica International, 2003, 42, 1, 115-129
dc.identifier.issn0016-7169
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/35064
dc.subjectWindward Passage
dc.subjectcurrent measurements
dc.subjectdata comparison
dc.titleA COMPARISON OF DIRECT OBSERVATIONS OF VELOCITY AND TRANSPORT IN THE WINDWARD PASSAGE
dc.typeСтатья

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