Influence of the coriolis force on the velocity structure of gravity currents in straight submarine channel systems

Journal of Geophysical Research: Oceans

Volumn 115, Issue 11, 2010, Pages

  Cossu, R ^a   Wells, M G ^a   Whlin, A K ^b  

^a UNIVERSITY OF TORONTO   (Canada)

^b UNIVERSITY OF GOTHENBURG   (Sweden)

Author keywords

[No Author keywords available]

Indexed keywords

BOUNDARY LAYERS; CORIOLIS FORCE; GRAVITATION; GRAVITY WAVES; LEVEES; OCEAN CURRENTS; SEDIMENT TRANSPORT; SUBMARINES; TURBIDITY;

ANALOG MODELS; CHANNEL VELOCITY; CHANNEL WIDTHS; CORIOLIS PARAMETER; EARTH'S ROTATION; EKMAN BOUNDARY LAYERS; EKMAN TRANSPORT; GRAVITY CURRENTS; INTERFACIAL BOUNDARY; LEVEE SYSTEM; NORTHERN HEMISPHERES; RETURN FLOW; ROSSBY NUMBERS; SUBMARINE CHANNEL; TRANSVERSE FLOW; TRANSVERSE VELOCITY; TURBIDITY CURRENT; VELOCITY STRUCTURE;

VELOCITY;

CORIOLIS FORCE; EKMAN LAYER; EKMAN TRANSPORT; FLOW PATTERN; GRAVITY FIELD; LEVEE; NORTHERN HEMISPHERE; NUMERICAL MODEL; ROSSBY NUMBER; SEDIMENT TRANSPORT; SUBMARINE CHANNEL; TURBIDITY CURRENT; VELOCITY STRUCTURE;

EID: 77956726502     PISSN: None     EISSN: 21699291     Source Type: Journal    
DOI: 10.1029/2010JC006208     Document Type: Article

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