Structure of the buoyant plume formed by O b and Y enisei river discharge in the southern part of the K ara S ea during summer and autumn-Reference-Cited by-同舟云学术

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Structure of the buoyant plume formed by O b and Y enisei river discharge in the southern part of the K ara S ea during summer and autumn

Published:2017-07 Issue:7 Volume:122 Page:5916-5935
ISSN:2169-9275
Container-title:Journal of Geophysical Research: Oceans
language:en
Short-container-title:J. Geophys. Res. Oceans

Author:

Osadchiev A. A.¹^ORCID,Izhitskiy A. S.¹,Zavialov P. O.¹,Kremenetskiy V. V.¹,Polukhin A. A.¹^ORCID,Pelevin V. V.¹,Toktamysova Z. M.²

Affiliation:

1. Shirshov Institute of Oceanology, Russian Academy of SciencesMoscow Russia

2. Higher School of EconomicsMoscow Russia

Funder

Russian Scientific Foundation

Publisher

American Geophysical Union (AGU)

Subject

Earth and Planetary Sciences (miscellaneous),Space and Planetary Science,Geochemistry and Petrology,Geophysics,Oceanography

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/2016JC012603

Reference73 articles.

1. Correlation of river water and local sea-ice melting on the Laptev Sea shelf (Siberian Arctic)

2. Discharge of the Changjiang (Yangtze River) into the East China Sea

3. Seasonal distribution of nutrients and primary productivity on the eastern continental shelf of Venezuela as influenced by the Orinoco River

4. Patos Lagoon outflow within the Río de la Plata plume using an airborne salinity mapper: Observing an embedded plume

5. Freshwater and its role in the Arctic Marine System: Sources, disposition, storage, export, and physical and biogeochemical consequences in the Arctic and global oceans

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