Atmospheric forcing of the Oregon coastal ocean during the 2001 upwelling season ...

Copyrighted by American Geophysical Union. Meteorological conditions during an intensive oceanographic observational program in May through August 2001 along the central Oregon coast are described and related to larger-scale and longer-term conditions. Southward wind stresses of 0.05-0.1 N m⁻² occur...

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Bibliographic Details
Main Authors: Bane, J. M., Levine, M. D., Boyd, T., Perlin, N., Kosro, P. M., Samelson, R. M., Meaux, M. F., Haines, S. M.
Format: Text
Language:English
Published: The University of North Carolina at Chapel Hill University Libraries 2005
Subjects:
Online Access:https://dx.doi.org/10.17615/vcdk-2j41
https://cdr.lib.unc.edu/concern/articles/47429j61w
Description
Summary:Copyrighted by American Geophysical Union. Meteorological conditions during an intensive oceanographic observational program in May through August 2001 along the central Oregon coast are described and related to larger-scale and longer-term conditions. Southward wind stresses of 0.05-0.1 N m⁻² occurred roughly 75% of the time, with a sustained period of dominantly southward stress from mid-June through July. Wind variations were correlated with variations in the large-scale Aleutian Low and North Pacific High pressure centers; correlations with the continental Thermal Low were small. Intraseasonal oscillations in alongshore wind stress (periods near 20 days) correlated with the north-south position of the jet stream. These stress oscillations drove 20 day oscillations in upper ocean temperature, with a lag of roughly 5 days for maximum correlation and amplitudes near 4°C. The sum of sensible and latent air-sea heat fluxes was generally into the atmosphere through June, then weakly into the ocean thereafter, ...