Abstract
Atmospheric-hydrodynamic coupling in the nearshore
Grupo de Dinámica de Flujos Ambientales, CEAMA-Universidad de Granada, Granada, Spain
Grupo de Dinámica de Flujos Ambientales, CEAMA-Universidad de Granada, Granada, Spain
Grupo de Dinámica de Flujos Ambientales, CEAMA-Universidad de Granada, Granada, Spain
Grupo de Dinámica de Flujos Ambientales, CEAMA-Universidad de Granada, Granada, Spain
Grupo de Dinámica de Flujos Ambientales, CEAMA-Universidad de Granada, Granada, Spain
Natural beach shorelines commonly present morphological rhythmic or non-rhythmic features of varying geometrical characteristics. Traditionally, their formation is believed to be due to wave-induced processes, a line thoroughly investigated during the last few decades. However, these natural beach formations are frequently bounded by coastal cliffs (or capes) and are affected by intense winds, a fact not previously considered. This paper presents the results of a field survey, demonstrating the existence of atmospheric-hydrodynamic coupling in the nearshore region outside of the breaking zone at Carchuna beach (Motril, Spain), where the atmospheric conditions are influenced by a lateral geographic obstacle (Cape Sacratif).
Received 17 September 2008; accepted 24 October 2008; published 2 December 2008.
Citation: (2008), Atmospheric-hydrodynamic coupling in the nearshore, Geophys. Res. Lett., 35, L23601, doi:10.1029/2008GL036043.
Cited By
