On the mid-depth circulation in the Labrador and Irminger Seas

Geophysical Research Letters

Volumn 28, Issue 18, 2001, Pages 3433-3436

  Kase R H ^a   Biastoch, A ^b   Stammer, D B ^b  

^a GEOMAR HELMHOLTZ CENTRE FOR OCEAN RESEARCH KIEL   (Germany)

^b UNIVERSITY OF CALIFORNIA   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

MATHEMATICAL MODELS; THERMAL PLUMES; SEA LEVEL;

SEA LEVEL DEPRESSION;

OCEANOGRAPHY; FLOW OF WATER;

BOTTOM TOPOGRAPHY; NUMERICAL MODEL; OCEANIC CIRCULATION; WIND FORCING;

IRMINGER SEA; LABRADOR SEA;

BOTTOM TOPOGRAPHY; DENMARK STRAIT; DENMARK STRAIT OVERFLOW WATERS; INDUCED FLOWS; MID-DEPTH CIRCULATION; NUMERICAL CIRCULATION MODEL; RECIRCULATION ZONES; RECIRCULATIONS;

LAVANDULA;

EID: 0035883379     PISSN: 00948276     EISSN: None     Source Type: Journal    
DOI: 10.1029/2001GL013192     Document Type: Article

References (16)

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3. Developments in ocean climate modelling
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5. Flow through Denmark strait
6. Mid-depth recirculation observed on the interior Labrador and Irminger seas by direct velocity measurements
7. Finite-volume, incompressible Navier Stokes model for studies of the ocean on parallel computers
8. Transient response in a z-level ocean model with bottom topography resolved using the method of partial cells
9. Generalized two-layer models of ocean circulation
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11. Surprisingly rapid spreading of newly formed intermediate waters across the North Atlantic Ocean
12. Circulation characteristics in three eddy-permitting models of the North Atlantic