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Marcus Sobarzo, Camila Soto-Riquelme, Raúl P. Flores and Gonzalo S. Saldías
The response of inner shelf circulation and bottom temperature variability to synoptic wind forcing and freshwater outflow is evaluated in an area with a wide continental shelf off central Chile. This forced circulation, with a strong seasonal evolution ...
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Mehmet Ilicak, Ivan Federico, Ivano Barletta, Sabri Mutlu, Haldun Karan, Stefania Angela Ciliberti, Emanuela Clementi, Giovanni Coppini and Nadia Pinardi
The Turkish Strait System, which is the only connection between the Black Sea and the Mediterranean Sea, is a challenging region for ocean circulation models due to topographic constraints and water mass structure. We present a newly developed high resol...
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KiRyong Kang and Guan-hong Lee
Flow measurements were performed in the altered Yeongsan estuary, Korea, in August 2011, to investigate changes in flow structure in the water column and turbulence characteristics very close to the bed. Comparison between the bottom turbulent kinetic en...
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Reza Marsooli, Philip M. Orton, James Fitzpatrick and Heather Smith
Using a validated coupled hydrodynamic-tracer transport model, this study quantified the mean residence time in Jamaica Bay, a highly eutrophic lagoonal estuary in New York City. The Bay is a well-mixed to partially-stratified estuary with heavily-dredge...
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Zhongfan Zhu, Xiaomei Bai, Jie Dou, Pengfei Hei
Pág. 1 - 23
Blue tides at the head of Tokyo Bay are a hydro-environmental phenomenon where seawater appears to be milky blue because of the reflection of the sunlight off surface water containing large amounts of sulphur particles. Its appearance is due to the coast...
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Ping Wang, Harry Wang, Lewis Linker and Kyle Hinson
Computer model experiments are applied to analyze hypoxia reductions for opposing wind directions under various speeds and durations in the north?south oriented, two-layer-circulated Chesapeake estuary. Wind?s role in destratification is the main mechani...
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S. N. BULGAKOV,YURI N. SKIBA
The classic Stommel (1961) model of thermohaline circulation has predicted the existence of two modes of ocean motion for the pole-equator system. These are, one-cell thermal and one-cell saline modes. In contrast, the laboratory experime...
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YURI N. SKIBA,S. N. BULGAKOV
A series of laboratory experiments with forced temperature and salinity were conducted using an apparatus (channel between pole and equator boxes) designed to duplicate the conceptual Stommel?s model of thermohaline circulation. The flow patterns are ...
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