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Volumn 39, Issue 6, 2009, Pages 1298-1316
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Coastal wind-driven circulation in the vicinity of a bank. Part II: Modeling flow over the Heceta Bank complex on the Oregon coast
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Author keywords
[No Author keywords available]
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Indexed keywords
BAROCLINIC;
BAROTROPIC;
BOTTOM BOUNDARY LAYER;
BOTTOM STRESS;
COASTAL UPWELLING;
COASTAL WINDS;
DENSE WATERS;
DENSITY FIELDS;
DEPTH CHANGES;
DOWN-WELLING;
EKMAN PUMPING;
FLOW BACK;
FLOW DIRECTION;
JET FLOW;
MODEL RESULTS;
MOMENTUM BALANCES;
NEAR-BOTTOM DENSITY;
NUMERICAL EXPERIMENTS;
OREGON COAST;
POTENTIAL VORTICITY;
RELATIVE VORTICITY;
SHALLOWER WATER;
SPATIAL VARIABILITY;
VERTICAL VELOCITY;
WHITNEY;
WIND-DRIVEN CIRCULATION;
ADVECTION;
LANDFORMS;
VORTICITY;
WIND;
WIND STRESS;
JETS;
ADVECTION;
AGEOSTROPHIC FLOW;
BENTHIC BOUNDARY LAYER;
BOTTOM STRESS;
CIRCULATION MODELING;
COASTAL CIRCULATION;
CONTINENTAL SHELF;
DOWNWELLING;
EKMAN PUMPING;
GEOSTROPHIC FLOW;
JET FLOW;
NEARSHORE DYNAMICS;
NUMERICAL MODEL;
POTENTIAL VORTICITY;
PRESSURE GRADIENT;
SPATIAL VARIATION;
SYMMETRY;
UPWELLING;
WIND STRESS;
WIND-DRIVEN CIRCULATION;
HECETA BANK;
OREGON SHELF;
PACIFIC OCEAN;
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EID: 67949111163
PISSN: 00223670
EISSN: None
Source Type: Journal
DOI: 10.1175/2008JPO3967.1 Document Type: Article |
Times cited : (6)
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References (10)
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