Lagrangian characteristics of continental shelf flows forced by periodic wind stress

The coastal ocean may experience periods of fluctuating along-shelf wind direction, causing shifts between upwelling and downwelling conditions with responses that are not symmetric. We seek to understand these asymmetries and their implications on the Eulerian and Lagrangian flows. We use a two-d...

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Bibliographic Details
Main Authors: B. T. Kuebel Cervantes, J. S. Allen, R. M. Samelson
Format: Article
Language:English
Published: Copernicus Publications 2004-01-01
Series:Nonlinear Processes in Geophysics
Online Access:http://www.nonlin-processes-geophys.net/11/3/2004/npg-11-3-2004.pdf

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