Wind-driven inertial waves observed during Phase III of GATE.

Käse, Rolf H. and Olbers, D. J. (1980) Wind-driven inertial waves observed during Phase III of GATE. Deep Sea Research Part A. Oceanographic Research Papers, 26A (Suppl. 1). pp. 217-224. DOI 10.1016/B978-1-4832-8366-1.50015-7.

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Abstract

Current and wind stress time series obtained from the F1-mooring are analysed with the aim of examining linear correspondences and testing the adequacy of linear coupling models at near-inertial frequencies. Significant linear correlations are found in the data set which are consistent with a linear winddriven model of the current system. The current in the mixed layer can be described by inertial oscillations directly forced by the local wind stress. A wind-driven simulation model of the mixed layer currents yields an energy input of 3.10-3 W/m2. The current in the thermocline can be described by a linear internal wave field of downward propagating wave groups driven via Ekman suction by the wind stress field. Internal waves are generated at a rate of 10-3 W/m2, consistently estimated from both kinematic and dynamic considerations.

Document Type: Article
Research affiliation: OceanRep > GEOMAR > FB1 Ocean Circulation and Climate Dynamics > FB1-TM Theory and Modeling
Refereed: Yes
Open Access Journal?: No
DOI etc.: 10.1016/B978-1-4832-8366-1.50015-7
ISSN: 0198-0149
Projects: GATE
Date Deposited: 17 Mar 2016 08:09
Last Modified: 22 Sep 2016 12:39
URI: http://oceanrep.geomar.de/id/eprint/31857

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