- Abstract:
-
The spreading of inertial oscillations induced by the passage of Hurricane Juan (2003) across the Gulf Stream and the Scotian Shelf is examined using a regional model of the northwest Atlantic Ocean. It is found that surface-intensified inertial oscillations develop at locations remote from the storm track after a period of 5-10 days. A diagnostic technique reveals the importance of advection by the background geostrophic flow for explaining this effect. The results suggest that advection by ...
Expand abstract - Publication status:
- Published
- Publisher copy:
- 10.1029/2004GL020084
-
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- Journal:
- GEOPHYSICAL RESEARCH LETTERS
- Volume:
- 31
- Issue:
- 14
- Publication date:
- 2004-07-30
- DOI:
- ISSN:
-
0094-8276
- URN:
-
uuid:4486e17c-6ed6-4aa6-8743-5da268a4b5e7
- Source identifiers:
-
160896
- Local pid:
- pubs:160896
- Language:
- English
- Copyright date:
- 2004
Journal article
Advective spreading of storm-induced inertial oscillations in a model of the northwest Atlantic Ocean
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