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Xia Huayong, Liu Changjian, Wang Dongxiao. The upwelling driven by the Zhujiang River runoff in 2006 summer[J]. Haiyang Xuebao, 2018, 40(7): 43-54. doi: 10.3969/j.issn.0253-4193.2018.07.004
Citation: Xia Huayong, Liu Changjian, Wang Dongxiao. The upwelling driven by the Zhujiang River runoff in 2006 summer[J]. Haiyang Xuebao, 2018, 40(7): 43-54. doi: 10.3969/j.issn.0253-4193.2018.07.004

The upwelling driven by the Zhujiang River runoff in 2006 summer

doi: 10.3969/j.issn.0253-4193.2018.07.004
  • Received Date: 2017-09-10
  • Rev Recd Date: 2017-12-22
  • A summer hydrologic survey in the Zhujiang River Estuary and its adjacent seas was performed in July and August, 2006. The survey data show that while a part of the diluted water from the Zhujiang River is transported eastwards by the overlying southwesterly monsoon, most of the diluted water is transported westwards off the coast of western Guangdong Province, and there is upwelling underlying the westwards spreading diluted water. In the existing modelling studies of the upwelling in the northern South China Sea, the upwelling does not occur off the Zhujiang River Estuary under the southwesterly monsoon, which demonstrates that the southwesterly monsoon should not be the major driving force of the upwelling off the Zhujiang River Estuary. As indicated by the distribution of sea water salinity and temperature, time series of currents from mooring observations and current fields from shipboard ADCP measurements, the major formation mechanism of upwelling ought to be:(1) the vertical gravitational circulations off the river mouth driven by the southwards spreading discharges; (2) the bottom boundary Ekman effect of the eastward coastal current beneath the density transition layer; and (3) the effect of mesoscale cool eddies among the diluted water bulges off the river mouths.
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