Zhai, Xiaoming, Greatbatch, Richard J. and Sheng, Jinyu (2004) Advective spreading of storm-induced inertial oscillations in a model of the northwest Atlantic Ocean. Geophysical Research Letters, 31 (14). ISSN 0094-8276
Full text not available from this repository. (Request a copy)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 mean circulation can play a role in redistributing near-inertial energy in the ocean. We argue that advective redistribution could have important consequences for understanding diapycnal mixing in the ocean.
Item Type: | Article |
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Faculty \ School: | Faculty of Science > School of Environmental Sciences |
UEA Research Groups: | Faculty of Science > Research Groups > Marine and Atmospheric Sciences (former - to 2017) Faculty of Science > Research Groups > Meteorology, Oceanography and Climate Dynamics (former - to 2017) Faculty of Science > Research Groups > Climate, Ocean and Atmospheric Sciences (former - to 2017) Faculty of Science > Research Groups > Centre for Ocean and Atmospheric Sciences |
Depositing User: | Pure Connector |
Date Deposited: | 23 Oct 2013 10:18 |
Last Modified: | 24 Oct 2022 04:50 |
URI: | https://ueaeprints.uea.ac.uk/id/eprint/43787 |
DOI: | 10.1029/2004GL020084 |
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