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Key Lab of Ocean Dynamic processes and Satellite Oceanography, State Oceanic Administration; Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012
The hydrodynamics in the Weihe River Estuary is analyzed by using a set data measured from May 1997 and June 1998 respectively. The results show that the estuary is micro-tidal, dominated by the M2 component. The salinity is raised and the temperature is decreased, as well as the occasion of gravitational circulation is reduced, as the currents are cutted in the upstream of the estuary by a sluice gate.
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