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...
Main Authors: | B. T. Kuebel Cervantes, J. S. Allen, R. M. Samelson |
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Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2004-01-01
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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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