Water Dynamics and Structure in the Estuary of the Partizanskaya River (Nakhodka Bay, Sea of Japan)
Water Resources, ISSN: 0097-8078, Vol: 46, Issue: 1, Page: 29-38
2019
- 3Citations
- 6Captures
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Example: if you select the 1-year option for an article published in 2019 and a metric category shows 90%, that means that the article or review is performing better than 90% of the other articles/reviews published in that journal in 2019. If you select the 3-year option for the same article published in 2019 and the metric category shows 90%, that means that the article or review is performing better than 90% of the other articles/reviews published in that journal in 2019, 2018 and 2017.
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Article Description
Abstract: Field studies of the seasonal and daily dynamics of the mixing zone were carried out in the microtidal estuary of the Partizanskaya River. The position of the mixing zone was determined by river runoff volume. The upstream boundary of the mixing zone was located at a distance from 5 (at river discharge of 73.67 m/s) to 12.5 km (at 7.7 m/s) from the mouth bar. The estuary features a two-layer water circulation, resulting in the formation of halocline with a gradient of water salinity of up to 30‰ per 1 m. Salinity variations at rifts, caused by tides, reach 27‰ over a 3-hour period.
Bibliographic Details
http://www.scopus.com/inward/record.url?partnerID=HzOxMe3b&scp=85063988917&origin=inward; http://dx.doi.org/10.1134/s0097807819010135; http://link.springer.com/10.1134/S0097807819010135; http://link.springer.com/content/pdf/10.1134/S0097807819010135.pdf; http://link.springer.com/article/10.1134/S0097807819010135/fulltext.html; https://dx.doi.org/10.1134/s0097807819010135; https://link.springer.com/article/10.1134/S0097807819010135
Pleiades Publishing Ltd
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