RT journal article
T1 Meteorologically forced subinertial flows and internal wave generation at the main sill of the Strait of Gibraltar
A1 Vázquez López-Escobar, Águeda
A1 Bruno Mejías, Miguel
A1 Izquierdo González, Alfredo
A1 Macías Moy, Diego
A1 Ruiz Cañavate, Antonio
A2 Biología
A2 Física Aplicada
K1 Subinertial flows
K1 Internal waves
K1 Stratified flow
K1 Internal bore
K1 Gibraltar Strait
K1 Internal hydraulic
AB The generation of large-amplitude internal waves in the Strait of Gibraltar is a widely known phenomenon. Those waves are produced by the interaction of barotropic tidal flow with the main sill (Camarinal Sill) topography and the stratified water column. That interaction primarily causes internal tides that evolve, by non-linear processes, into large-amplitude (more than 100m) internal waves exhibiting much shorter oscillation periods than those related to the basic tidal variability. Recent observations have shown that on many occasions large-amplitude internal wave generation is dependent on the state of the subinertial flows, which are basically driven by the atmospheric pressure fluctuations over the Mediterranean. Therefore, depending on the meteorological situation over the Mediterranean, internal wave events may be inhibited or activated. (c) 2008 Elsevier Ltd. All rights reserved.
YR 2008
FD 2008-01-03
LK http://hdl.handle.net/10498/19754
UL http://hdl.handle.net/10498/19754
LA eng
DS Repositorio Institucional de la Universidad de Cádiz
RD 13-nov-2026