Journal
JOURNAL OF PHYSICAL OCEANOGRAPHY
Volume 46, Issue 8, Pages 2403-2410Publisher
AMER METEOROLOGICAL SOC
DOI: 10.1175/JPO-D-16-0040.1
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Funding
- National Basic Research Program of China [2013CB430301, 2013CB430303]
- NSFC [41276023, 41376022, 41125019, 41521005]
- [GASI-IPOVAI-04]
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The three-dimensional responses of a cyclonic ocean eddy (COE) for 1-2 months following a typhoon were investigated using altimeter data and numerical experiments. Two significant features were found: 1) the cyclonic eddy was enhanced, and the three-dimensional structure was changed, and 2) the cyclonic eddy underwent two processes: elliptical deformation and reaxisymmetrization in the horizontal plane. These two features are generally associated with typhoon-induced upwelling and the dynamic processes of eddy adjustment. These results imply that the local ocean processes can be affected by a typhoon through low-frequency response.
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