Nonlinear aspects of shelf waves and mean currents

2008 ◽  
pp. 206-211
Author(s):  
R. H. J. Grimshaw
Keyword(s):  
Shelf Waves

scholarly journals Hydraulic control of continental shelf waves

2021 ◽  
Vol 917 ◽  
Author(s):  
S. Jamshidi ◽  
E.R. Johnson
Keyword(s):  
Continental Shelf ◽  
Hydraulic Control ◽  
Shelf Waves ◽  
Continental Shelf Waves

Abstract

Corrigendum to “Continental shelf waves on the Alborán sea” [Cont. Shelf Res. 111 (2015) 1–8]

2016 ◽  
Vol 127 ◽  
pp. 43
Author(s):  
M.A. Serrano ◽  
M. Díez-Minguito ◽  
M. Ortega-Sánchez ◽  
M.A. Losad
Keyword(s):  
Continental Shelf ◽  
Alboran Sea ◽  
Shelf Waves ◽  
Continental Shelf Waves ◽  
Alborán Sea

Continental shelf waves and their influence on the circulation around the Great Barrier Reef

1983 ◽  
Vol 34 (1) ◽  
pp. 23 ◽  
Author(s):  
E Wolanski ◽  
AF Bennett
Keyword(s):  
Continental Shelf ◽  
Great Barrier Reef ◽  
Sea Level ◽  
Atmospheric Pressure ◽  
Low Frequency ◽  
Internal Tides ◽  
Wind Component ◽  
Barrier Reef ◽  
Longshore Current ◽  
Shelf Waves

Winds and atmospheric pressure, sea level and water currents were measured at several locations over the continental shelf, both east and west of the Great Barrier Reef, between 14.5�s. and 20�S., from June to November 1980. The dominant wind direction changed from westward over the Coral Sea to north- westward (roughly parallel to the shore) over the shelf. A strong non-tidal low-frequency signal in all sea- level and longshore current data was found, highly coherent from site to site and strongly correlated with the longshore wind component over the shelf, though not with the atmospheric pressure. A model of wind- driven barotropic shelf waves is used to explain a number of observations, such as the invariance of temporal fluctuations of longshore current with distance from shore, and the northward longshore propagation of oceanic disturbances at a speed equal to twice that of the first-mode barotropic free shelf wave, a speed one order of magnitude smaller than that of the wind system. The low-frequency current fluctuations resulted in large water displacements, up and down the coast. Low-frequency cross-shelf currents were much weaker and less coherent. Two upwelling mechanisms are internal tides and internal Kelvin waves coupled to the barotropic shelf waves.

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