A Three Dimensional Circulation Model of the South China Sea
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Cited by (56)
Long-term changes of South China Sea surface temperatures in winter and summer
2017, Continental Shelf ResearchCitation Excerpt :They suggested that the summer monsoon weakened, thus reducing the upwelling east of Vietnam and warming the area. The upwelling is a localized phenomenon due to the southwesterly wind along the coast (Chen et al., 2012; Pohlmann, 1987), so scrutiny of the local wind is necessary. More importantly, as we will display later, another part of the SCS showed stronger warming, but this phenomenon was not investigated.
Assessment and analysis of the chlorophyll-a concentration variability over the Vietnamese coastal waters from the MERIS ocean color sensor (2002–2012)
2017, Remote Sensing of EnvironmentCitation Excerpt :The tidal energy is dissipated in the ESV by the bottom friction in shallow areas and by the scattering of surface tide into internal tides (Zu et al., 2008). The ESV is strongly influenced by the periodic semi-annual reversing circulation of the atmosphere associated to the monsoon regime (Pohlmann, 1987). In winter northeasterly wind dominate with an average velocity of 9 m s− 1 over Vietnam (October–April).
Inter-annual variability of upwelling off the South-Vietnamese coast and its relation to nutrient dynamics
2013, Global and Planetary ChangeCitation Excerpt :Both deduced the surface currents from ship drift data and prevailing wind data. Pohlmann (1987) applied the first prognostic baroclinic three-dimensional circulation model to simulate the SCS circulations during the winter and summer monsoons, more or less the same did Mao et al. (1992). Li et al. (1992a,b,1994), Liu and Su (1992), Zeng et al. (1989) and Zeng et al. (1992) used two-dimensional numerical models to calculate the monthly or seasonal mean SCS circulation.
Modelling the circulation on the continental shelf of the province Khanh Hoa in Vietnam
2009, Journal of Marine Systems