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The structure of subtidal currents within and around Lydonia Canyon: evidence for enhanced cross-shelf fluctuations over the mouth of the canyon

Journal of Geophysical Research

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Abstract

The Coriolis force on the cross-canyon flow, turbulent Reynolds stresses, and acceleration of the along-canyon flow balanced the imposed pressure gradient for flow near the rim of Lydonia Canyon. The Coriolis force was not important in the deeper portions of the canyon, where baroclinic adjustments of the density field began to be an important factor in the momentum balance. -from Authors

Additional Publication Details

Publication type:
Article
Publication Subtype:
Journal Article
Title:
The structure of subtidal currents within and around Lydonia Canyon: evidence for enhanced cross-shelf fluctuations over the mouth of the canyon
Series title:
Journal of Geophysical Research
Volume
94
Issue:
C6
Year Published:
1989
Language:
English
Larger Work Type:
Article
Larger Work Subtype:
Journal Article
Larger Work Title:
Journal of Geophysical Research
First page:
8091
Last page:
8110
Number of Pages:
20