Intensification of deep-water circulation in a mesoscale basin under the influence of the bottom topography

Physical Oceanography

Volumn 15, Issue 2, 2005, Pages 71-78

  Korotaev, G K ^a  

^a INSTITUTE OF HYDROBIOLOGY   (Ukraine)

Author keywords

[No Author keywords available]

Indexed keywords

CATCHMENTS; MATHEMATICAL MODELS; OCEANOGRAPHY; SEAWATER; WIND EFFECTS;

AIR-SEA INTERACTION; DEEP WATER; MODELING; TOPOGRAPHY; WIND-DRIVEN CIRCULATION;

BLACK SEA; EURASIA;

EID: 33646261378     PISSN: 09285105     EISSN: 09285105     Source Type: Journal    
DOI: 10.1007/s11110-005-0031-4     Document Type: Article

References (3)

1. A. S. Sarkisyan and V. F. Ivanov, "Combined effect of baroclinity and bottom topography as an important factor in the dynamics of sea currents," Izv. Akad. Nauk SSSR, Fiz. Atmosf. Okean., 7, No.2, 173-188 (1971).
2. V. N. Zyryanov, Theory of Steady Oceanic Currents [in Russian], Gidrometeoizdat, Leningrad (1985).
3. G. K. Korotaev and N. B. Shapiro, "On the influence of bottom topography on the oceanic circulation (a two-layer model)," Morsk. Gidrofiz. Issled., No. 5(55), 58-72 (1971).