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Impacts of wind forcing on sea level variations in the East China Sea: Local and remote effects
- Source :
- Journal of Marine Systems. 154:172-180
- Publication Year :
- 2016
- Publisher :
- Elsevier BV, 2016.
-
Abstract
- The regional sea level variation in the East China Sea (ECS) was influenced not only by local factors but also by remote wind from adjoining ocean with the oceanic connectivity influenced by upper-ocean circulation. The satellite altimeter observations showed that from 1993 to 2008, the inter-annual sea level variation in the ECS was negatively related to the strength of Kuroshio. To investigate the relative role of local and remote wind, two sensitive experiments were carried out using the POP model. Model experiments revealed that wind-induced redistributions of water played a significant role in the sea level variation of the ECS. The seasonal variations were induced by both local winds and remote Pacific wind stress with approximately equal contribution. However, on the inter-annual sea level variations, the remote wind forcing over the North Pacific could contribute substantially more than that of local wind which modulated sea level immediately. Remote wind influenced the China Sea in forms of changing of wind stress curl and ocean currents, which influenced the intensity of the Kuroshio, especially during El Nino episodes. (C) 2015 Elsevier B.V. All rights reserved.
- Subjects :
- integumentary system
010504 meteorology & atmospheric sciences
010505 oceanography
Wind stress curl
Ocean current
Wind stress
Aquatic Science
Oceanography
01 natural sciences
Satellite altimeter
Sea breeze
Climatology
Environmental science
Ecology, Evolution, Behavior and Systematics
Sea level
0105 earth and related environmental sciences
Wind forcing
China sea
Subjects
Details
- ISSN :
- 09247963
- Volume :
- 154
- Database :
- OpenAIRE
- Journal :
- Journal of Marine Systems
- Accession number :
- edsair.doi...........a0903fb90e734dfc92b47cca435e0486
- Full Text :
- https://doi.org/10.1016/j.jmarsys.2015.10.009