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FILLING OF THE MARMARA SEA BY THE DARDANELLES LOWER LAYER INFLOW
Date
1993-09-01
Author
BESIKTEPE, S
OZSOY, E
UNLUATA, U
Metadata
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The sub-halocline waters of the Marmara Sea are renewed with the incoming Dardanelles lower layer flow. As shown by observations, this inflow takes the form of a turbulent plume which first sinks down and then spreads out into the interior. A ''filling box'' model is developed to test the sensitivity of the Dardanelles-Marmara Sea system to the set of relevant environmental parameters. The seasonal variability of the Dardanelles inflow is shown to play a crucial role in the sub-halocline water mass characteristics of the Marmara Sea.
Subject Keywords
Circulation
,
Ocean
,
Model
URI
https://hdl.handle.net/11511/66843
Journal
DEEP-SEA RESEARCH PART I-OCEANOGRAPHIC RESEARCH PAPERS
DOI
https://doi.org/10.1016/0967-0637(93)90034-z
Collections
Graduate School of Marine Sciences, Article
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S. BESIKTEPE, E. OZSOY, and U. UNLUATA, “FILLING OF THE MARMARA SEA BY THE DARDANELLES LOWER LAYER INFLOW,”
DEEP-SEA RESEARCH PART I-OCEANOGRAPHIC RESEARCH PAPERS
, pp. 1815–1838, 1993, Accessed: 00, 2020. [Online]. Available: https://hdl.handle.net/11511/66843.