Articles | Volume 16, issue 4
https://doi.org/10.5194/os-16-781-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/os-16-781-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Influence of estuarine tidal mixing on structure and spatial scales of large river plumes
Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow, Russia
Institute of Geology of Ore Deposits, Petrography, Mineralogy and
Geochemistry, Russian Academy of Sciences, Moscow, Russia
Moscow Institute of Physics and Technology, Dolgoprudny, Russia
Igor Medvedev
Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow, Russia
Fedorov Institute of Applied Geophysics, Roshydromet, Moscow, Russia
Sergey Shchuka
Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow, Russia
Moscow Institute of Physics and Technology, Dolgoprudny, Russia
Mikhail Kulikov
Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow, Russia
Eduard Spivak
Ilyichov Pacific Oceanological Institute, Far Eastern Branch of the
Russian Academy of Sciences, Vladivostok, Russia
Maria Pisareva
Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow, Russia
Igor Semiletov
Ilyichov Pacific Oceanological Institute, Far Eastern Branch of the
Russian Academy of Sciences, Vladivostok, Russia
National Research Tomsk Polytechnic University, Tomsk, Russia
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23 citations as recorded by crossref.
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- Rare Earth Elements in Sediments from the Laptev Sea Shelf: Insight into Sources and Distribution Factors A. Ruban et al. 10.3390/quat7010012
- Structure and variability of the Pechora plume in the southeastern part of the Barents Sea V. Rogozhin et al. 10.3389/fmars.2023.1052044
- Mesoscale Eddy Chain Structures in the Black Sea and Their Interaction with River Plumes: Numerical Modeling and Satellite Observations K. Korotenko et al. 10.3390/rs15061606
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- Biogeochemical Markers to Identify Spatiotemporal Gradients of Phytoplankton across Estuaries A. Egoda Gamage et al. 10.3390/coasts4030024
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- Fluorescent signatures of autochthonous dissolved organic matter production in Siberian shelf seas A. Drozdova et al. 10.3389/fmars.2022.872557
- Structure and Variability of the Lena River Plume in the South-Eastern Part of the Laptev Sea E. Spivak et al. 10.1134/S000143702106014X
- CDOM Optical Properties and DOC Content in the Largest Mixing Zones of the Siberian Shelf Seas A. Drozdova et al. 10.3390/rs13061145
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23 citations as recorded by crossref.
- The roles of river discharge and sea ice melting in formation of freshened surface layers in the Kara, Laptev, and East Siberian seas A. Osadchiev et al. 10.3389/fmars.2024.1348450
- Macrozoobenthos of the Pechora Bay in 2020–2021 indicates a likely change of common bivalve molluscs in the Arctic estuary A. Gebruk et al. 10.1007/s00300-023-03138-4
- Numerical Modeling of Extreme Sea Levels on the Laptev Sea Coast M. Kulikov et al. 10.3390/geosciences14090245
- Large River Plumes Detection by Satellite Altimetry: Case Study of the Ob–Yenisei Plume D. Frey & A. Osadchiev 10.3390/rs13245014
- Ice-dominated Arctic deltas I. Overeem et al. 10.1038/s43017-022-00268-x
- Data‐Driven Method With Numerical Model: A Combining Framework for Predicting Subtropical River Plumes W. Lu et al. 10.1029/2021JC017925
- Improved sea surface salinity data for the Arctic Ocean derived from SMAP satellite data using machine learning approaches A. Savin et al. 10.3389/fmars.2024.1358882
- Production of Fluorescent Dissolved Organic Matter by Microalgae Strains from the Ob and Yenisei Gulfs (Siberia) N. Lobus et al. 10.3390/plants11233361
- Influence of Riverine Discharge and Timing of Ice Retreat on Particle Sedimentation Patterns on the Laptev Sea Shelf A. Drits et al. 10.1029/2021JC017462
- Spreading and Transformation of River Discharge in the Arctic Ocean A. Osadchiev 10.1134/S1019331621060101
- Abundance, Biomass, and Production of Bacterioplankton at the End of the Growing Season in the Western Laptev Sea: Impact of Khatanga River Discharge (Arctic) A. Kopylov et al. 10.3390/jmse11081573
- Rare Earth Elements in Sediments from the Laptev Sea Shelf: Insight into Sources and Distribution Factors A. Ruban et al. 10.3390/quat7010012
- Structure and variability of the Pechora plume in the southeastern part of the Barents Sea V. Rogozhin et al. 10.3389/fmars.2023.1052044
- Mesoscale Eddy Chain Structures in the Black Sea and Their Interaction with River Plumes: Numerical Modeling and Satellite Observations K. Korotenko et al. 10.3390/rs15061606
- Satellite-Based Evaluation of Submarine Permafrost Erosion at Shallow Offshore Areas in the Laptev Sea A. Osadchiev et al. 10.3390/rs15205065
- Direct Salinity Effect on Absorbance and Fluorescence of Chernozem Water-Extractable Organic Matter V. Kholodov et al. 10.1007/s10498-024-09423-w
- Biogeochemical Markers to Identify Spatiotemporal Gradients of Phytoplankton across Estuaries A. Egoda Gamage et al. 10.3390/coasts4030024
- Complex interactions of ENSO and local conditions buffer the poleward shift of migratory fish in a subtropical seascape S. Vollrath et al. 10.1016/j.scitotenv.2023.165129
- Hydrophysical Structure and Current Dynamics of the Kodor River Plume A. Osadchiev et al. 10.1134/S000143702101015X
- Fluorescent signatures of autochthonous dissolved organic matter production in Siberian shelf seas A. Drozdova et al. 10.3389/fmars.2022.872557
- Structure and Variability of the Lena River Plume in the South-Eastern Part of the Laptev Sea E. Spivak et al. 10.1134/S000143702106014X
- CDOM Optical Properties and DOC Content in the Largest Mixing Zones of the Siberian Shelf Seas A. Drozdova et al. 10.3390/rs13061145
- Influence of the Coriolis Force on Spreading of River Plumes A. Osadchiev et al. 10.3390/rs15133397
Latest update: 10 Dec 2024
Short summary
The Yenisei and Khatanga rivers are among the largest estuarine rivers that inflow to the Arctic Ocean. Discharge of the Yenisei River is 1 order of magnitude larger than that of the Khatanga River. However, spatial scales of buoyant plumes formed by freshwater runoff from the Yenisei and Khatanga gulfs are similar. This feature is caused by intense tidal mixing in the Khatanga Gulf, which causes formation of the diluted and therefore anomalously deep and large Khatanga plume.
The Yenisei and Khatanga rivers are among the largest estuarine rivers that inflow to the Arctic...