Dynamics of upwelling annual cycle in the equatorial Atlantic Ocean
Journal Article
·
· Geophysical Research Letters
- National Taiwan Normal Univ., Taipei (Taiwan). Dept. of Earth Sciences; Academia Sinica, Taipei (Taiwan). Research Center for Environmental Change; University of Hawaii
- Univ. of Hawaii at Manoa, Honolulu, HI (United States)
- National Taiwan Normal Univ., Taipei (Taiwan). Dept. of Earth Sciences; Academia Sinica, Taipei (Taiwan). Research Center for Environmental Change
- Academia Sinica, Taipei (Taiwan). Research Center for Environmental Change
The annual upwelling is an important component of the equatorial Atlantic annual cycle. A simple theory is proposed using the framework of Zebiak-Cane (ZC) ocean model for insights into the dynamics of the upwelling annual cycle. It is demonstrated that in the Atlantic equatorial region this upwelling is dominated by Ekman processing in the west, whereas in the east it is primarily owing to shoaling and deepening of the thermocline resulting from equatorial mass meridional recharge/discharge and zonal redistribution processes associated with wind-driven equatorial ocean waves. This wind-driven wave upwelling plays an important role in the development of the annual cycle in the sea surface temperature of the cold tongue in the eastern equatorial Atlantic.
- Research Organization:
- Univ. of Hawaii, Honolulu, HI (United States)
- Sponsoring Organization:
- Ministry of Science and Technology (MOST); USDOE; USDOE Office of Science (SC)
- Grant/Contract Number:
- SC0005110
- OSTI ID:
- 1465347
- Alternate ID(s):
- OSTI ID: 1374445
- Journal Information:
- Geophysical Research Letters, Journal Name: Geophysical Research Letters Journal Issue: 8 Vol. 44; ISSN 0094-8276
- Publisher:
- American Geophysical UnionCopyright Statement
- Country of Publication:
- United States
- Language:
- English
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