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Russian Meteorology and Hydrology

, Volume 44, Issue 10, pp 667–673 | Cite as

Evolution of Suspended Sediment Budget in the Deltas of Lake Baikal Tributaries

  • S. R. ChalovEmail author
  • T. G. Potemkina
  • M. P. Pashkina
  • N. S. Kasimov
Article
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Abstract

The monitoring, field, and satellite datasets are used to estimate changes in suspended sediment budget for the Selenga and Upper Angara river deltas. Sediment deficit during recent decades dominates delta evolution due to decrease in the sediment delivery to the delta since the middle of the 1970s by 51% for the Selenga River and by 70% for the Upper Angara River. The observed decline in the sediment runoff and peak water flows associated with the sediment deposition within the inundated flood-plain of the deltas leads to the reduction of the sediment aggradation rates over both deltas. Under low water flows we observed longitudinal increase of the sediment transport rates along Selenga River delta; the Upper Angara constantly reduces sediment transport rates under various hydrological conditions.

Keywords

Suspended sediment budget delta Lake Baikal tributaries Selenga River Upper Angara River 

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References

  1. 1.
    N. I. Alekseevskii, Formation and Movement of River Sediments. (MGU, Moscow, 1998) [in Russian].Google Scholar
  2. 2.
    M. A. Glazovskaya, “Geochemical Barriers in Plain Solis, Their Typology, Functional Features, and Environmental Value,” Vestnik Moskovskogo Universiteta, Ser. 5, Geografiya, No. 1 (2012) [in Russian].Google Scholar
  3. 3.
    A. P. Lisitsyn, “The Marginal Filter of the Ocean,” Okeanologiya, No. 5, 34 (1994) [Oceanology, No. 5, 34 (1994)].Google Scholar
  4. 4.
    T. G. Potemkina, “Hydrological-morphological Zoning of the Mouth Zone of the Selenga River,” Vodnye Resursy, No. 1, 31 (2004) [Water Resour., No. 1, 31 (2004)].CrossRefGoogle Scholar
  5. 5.
    M. K. Tarasov and O. V. Tutubalina, “A Method for Determination of Water Turbidity in the Selenga River and in the Adjoining Area of Lake Baikal Using Remote Sensing Data,” Issledovanie Zemli iz Kosmosa, No. 1 (2018) [in Russian].Google Scholar
  6. 6.
    Erosion-channel Systems, Ed. by R. S. Chalov, A. Yu. Sidorchuk, and V. N. Golosov (INFRA-M, Moscow, 2017) [in Russian].Google Scholar
  7. 7.
    N. I. Alexeevsky, R. S. Chalov, K. M. Berkovich, and S. R. Chalov, “Channel Changes in Largest Russian Rivers: Natural and Anthropogenic Effects,” Int. J. River Basin Management, No. 2, 11 (2013).CrossRefGoogle Scholar
  8. 8.
    S. R. Chalov, V. O. Bazilova, and M. K. Tarasov, “Suspended Sediment Balance in Selenga Delta at the Late XX-Early XXI Century: Simulation by LANDSAT Satellite Images,” Water Resour., No. 3, 44 (2017).CrossRefGoogle Scholar
  9. 9.
    S. R. Chalov, J. Jarsjo, N. S. Kasimov, A. O. Romanchenko, J. Pietron, J. Thorslund, and E. V. Promakhova, “Spatio-temporal Variation of Sediment Transport in the Selenga River Basin, Mongolia and Russia,” Environ. Earth Sci., No. 2, 73 (2014).Google Scholar
  10. 10.
    S. Chalov, J. Thorslund, N. Kasimov, D. Aybulatov, E. Ilyicheva, D. Karthe, A. Kositsky, M. Lychagin, J. Nittrouer, M. Pavlov, J. Pietron, G. Shinkareva, M. Tarasov, E. Garmaev, Y. Akhtman, and J. Jarsjo, “The Selenga River Delta: A Geochemical Barrier Protecting Lake Baikal Waters,” Regional Environ. Change, No. 7, 17 (2017).Google Scholar
  11. 11.
    G. Chander, B. L. Markham, and D. L. Helder, “Summary of Current Radiometric Calibration Coefficients for Landsat MSS, TM, ETM+, and EO-1 ALI Sensors,” Remote Sens. Environ., No. 5, 113 (2009).CrossRefGoogle Scholar
  12. 12.
    T. Y. Dong, J. A. Nittrouer, M. J. Czapiga, H. Ma, B. McElroy, E. Il’icheva, M. Pavlov, S. Chalov, and G. Parker, “Roles of Bank Material in Setting Bankfull Hydraulic Geometry as Informed by the Selenga River Delta, Russia,” Water Resour. Res., 54 (2019).Google Scholar
  13. 13.
    N. L. Frolova, P. A. Belyakova, V. Yu. Grigoriev, A. A. Sazonov, L. V. Zotov, and J. Jarsjo, “Runoff Fluctuations in the Selenga River Basin,” Regional Environ., Change, 17 (2017).CrossRefGoogle Scholar
  14. 14.
    A. N. Gelfan and T. D. Millionschikova, “Validation of a Hydrological Model Intended for Impact Study: Problem Statement and Solution Example for Selenga River Basin,” Water Resour., No. 1, 45 (2018).CrossRefGoogle Scholar
  15. 15.
    E. Park and E. M. Latrubesse, “Modeling Suspended Sediment Distribution Patterns of the Amazon River Using MODIS Data,” Remote Sens. Environ., 147 (2014).CrossRefGoogle Scholar
  16. 16.
    T. M. Pavelsky and L. C. Smith, “Remote Sensing of Suspended Sediment Concentration, Flow Veiocity, and Lake Recharge in the Peace-Athabasca Delta, Canada,” Water Resour. Res., 45 (2009).Google Scholar
  17. 17.
    J. Pietron, J. Nittrouer, S. Chalov, T. Dong, N. Kasimov, G. Shinkareva, and J. Jarsjo, “Sedimentation Patterns in the Selenga River Delta under Changing Hydroclimatic Conditions,” Hydrol. Processes, No. 2, 32 (2018).CrossRefGoogle Scholar
  18. 18.
    T. G. Potemkina, “Sediment Runoff Formation Trends of Major Tributaries of Lake Baikal in the 20th Century and at the Beginning of the 21st Century,” Russ. Meteorol. Hydrol., No. 12, 36 (2011).Google Scholar
  19. 19.
    T. G. Potemkina and V. L. Potemkin, “Sediment Load of the Main Rivers of lake Baikal in a Changing Environment (East Siberia, Russia),” Quat. Int., 380-381 (2015).Google Scholar
  20. 20.
    K. G. Ruddick, V. de Cauwer, Y. Park, and G. Moore, “Seaborne Measurements of Near Infrared Water-leaving Reflectance: The Similarity Spectrum for Turbid Waters,” Limnol. Oceanogr., No. 2, 51 (2006).CrossRefGoogle Scholar
  21. 21.
    A. Tejedor, A. Longjas, I. Zaliapin, and E. Foufoula-Georgiou, “Delta Channel Networks: 1. A Graph-theoretic Approach for Studying Connectivity and Steady State Transport on Deltaic Surfaces,” Water Resour. Res., No. 6, 51 (2015).CrossRefGoogle Scholar

Copyright information

© Allerton Press, Inc. 2019

Authors and Affiliations

  • S. R. Chalov
    • 1
    Email author
  • T. G. Potemkina
    • 2
  • M. P. Pashkina
    • 1
  • N. S. Kasimov
    • 1
  1. 1.Lomonosov Moscow State UniversityLeninskie Gory, MoscowRussia
  2. 2.Limnological Institute, Siberian BranchRussian Academy of SciencesIrkutskRussia

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