3D Numerical Modeling of Stratified Flows: Case Study of the Bosphorus Strait

dc.contributor.author	Mehmet
dc.contributor.author	Öztürk
dc.contributor.author	Berna
dc.contributor.author	Ayat
dc.contributor.author	Burak
dc.contributor.author	Aydoğan
dc.contributor.author	Yalçın
dc.contributor.author	Yüksel
dc.date.accessioned	2017-05-08T22:04:10Z
dc.date.available	2017-05-08T22:04:10Z
dc.date.copyright	September 2012
dc.date.issued	2012
dc.identifier.other	%28asce%29ww%2E1943-5460%2E0000177.pdf
dc.identifier.uri	http://yetl.yabesh.ir/yetl/handle/yetl/70413
dc.description.abstract	The Bosphorus Strait is a typical example of a narrow sea strait and, in general, has a two-layer flow structure. Driven by the water level difference between the Black Sea (north) and the Sea of Marmara (south), a lighter upper layer flows from north to south. A denser lower layer flow is caused by the density difference between the adjacent seas and flows in the opposite direction. In this study, the three-dimensional (3D) flow structure of the Bosphorus strait was modeled using the MIKE 3 hydrodynamic numerical code. Selecting the drag coefficient
dc.publisher	American Society of Civil Engineers
dc.title	3D Numerical Modeling of Stratified Flows: Case Study of the Bosphorus Strait
dc.type	Journal Paper
dc.journal.volume	138
dc.journal.issue	5
dc.journal.title	Journal of Waterway, Port, Coastal, and Ocean Engineering
dc.identifier.doi	10.1061/(ASCE)WW.1943-5460.0000132
dc.tree	Journal of Waterway, Port, Coastal, and Ocean Engineering:;2012:;Volume ( 138 ):;issue: 005
dc.contenttype	Fulltext