| dc.contributor.author | LATIF, MA | |
| dc.contributor.author | OZSOY, E | |
| dc.contributor.author | OGUZ, T | |
| dc.contributor.author | SUR, Halil İbrahim | |
| dc.contributor.author | UNLUATA, U | |
| dc.contributor.author | BESIKTEPE, ST | |
| dc.date.accessioned | 2021-03-04T11:28:51Z | |
| dc.date.available | 2021-03-04T11:28:51Z | |
| dc.date.issued | 1994 | |
| dc.identifier.citation | BESIKTEPE S., SUR H. İ. , OZSOY E., LATIF M., OGUZ T., UNLUATA U., "THE CIRCULATION AND HYDROGRAPHY OF THE MARMARA SEA", PROGRESS IN OCEANOGRAPHY, cilt.34, sa.4, ss.285-334, 1994 | |
| dc.identifier.issn | 0079-6611 | |
| dc.identifier.other | vv_1032021 | |
| dc.identifier.other | av_728eb2ed-849f-4fb0-a88c-9b0be700fd91 | |
| dc.identifier.uri | http://hdl.handle.net/20.500.12627/78851 | |
| dc.identifier.uri | https://doi.org/10.1016/0079-6611(94)90018-3 | |
| dc.description.abstract | A comprehensive set of data collected during 1986-1992 reveal seasonal and interannual variability in the circulation and hydrography of the Marmara Sea. Waters, which have contrasting properties and originate from the adjacent basins, supply the two-layer stratified flows in the Sea of Marmara. Turbulent entrainment into the upper layer in the exit region of the Bosphorus jet, and wind-stirring in winter, both contribute equally to the basin vertical mixing. | |
| dc.language.iso | eng | |
| dc.subject | Deniz Bilimleri ve Teknolojisi | |
| dc.subject | Fiziksel Oşinografi | |
| dc.subject | Mühendislik ve Teknoloji | |
| dc.subject | Oşinografi | |
| dc.subject | Temel Bilimler (SCI) | |
| dc.subject | Yerbilimleri | |
| dc.subject | OŞİNOGRAFİ | |
| dc.title | THE CIRCULATION AND HYDROGRAPHY OF THE MARMARA SEA | |
| dc.type | Makale | |
| dc.relation.journal | PROGRESS IN OCEANOGRAPHY | |
| dc.contributor.department | Dokuz Eylül Üniversitesi , , | |
| dc.identifier.volume | 34 | |
| dc.identifier.issue | 4 | |
| dc.identifier.startpage | 285 | |
| dc.identifier.endpage | 334 | |
| dc.contributor.firstauthorID | 14452 | |
