Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
4537731 | Deep Sea Research Part II: Topical Studies in Oceanography | 2006 | 15 Pages |
Abstract
An array of five buoys and three coastal stations is used to characterize the winds, stress, and curl of the wind stress over the shelf off Bodega Bay, California. The wind and wind stress are strong and persistent in the summer and weak in the winter. In the summer, wind and stress decrease strongly across the shelf, toward the coast. Combinations of buoys are used to compute the curl of the wind stress over different portions of the shelf. The mean summer 2001 curl of the wind stress over the array depends upon the area selected, varying between â1.32Ã10â6 and +7.80Ã10â6 Pa mâ1. The winter 2002 wind-stress curl also depends on location, varying from â2.06Ã10â6 to +2.78Ã10â6 Pa mâ1. Mean monthly curl of the wind stress is a maximum in the summer and a minimum near zero in the winter. In both the summer and the winter, the correlation between the wind-stress curl for different portions of the shelf varies between moderate negative, though insignificance, to high positive. A wind measurement at a single point can be poorly related to the measured curl of the wind stress at other locations over the shelf. The measurements show that the use of one wind measurement to characterize the curl of the wind stress over the shelf without further investigation of the local wind-stress curl structure is risky.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geology
Authors
Clive E. Dorman, Edward P. Dever, John Largier, Darko KoraÄin,