Dynamics and water structures in the estuary of the Partizanskaya river (Nakhodka Bay, Sea of Japan)
Keyword(s):
Run Off
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Herein, we report field studies of the seasonal and daily dynamics of the mixing zone in the micro-tidal mouth of the Partizanskaya river. The position of the mixing zone was determined according to the volume of river run-off. The upper boundary of the mixing zone was observed at 5 (at a river run-off of 73.67 m3/s) to 12.5 km (at 7.7 m3/s) from the mouth bar. The estuary is characterized by a two-layer circulation of water, which results in a halocline with a salinity gradient of up to 30% per 1 m. Variations of salinity in the rifts caused by tides reaches 27% over 3 h.
2015 ◽
Vol 8
(6)
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pp. 772-779
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1994 ◽
Vol 21
(1)
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pp. 141-155
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2000 ◽
Vol 26
(5)
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pp. 338-341
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1999 ◽
Vol 38
(5-6)
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pp. 255-286
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