Proceedings of IAHS
Proceedings of IAHS
PIAHS
Articles | Volume 375
Articles | Volume 375
https://doi.org/10.5194/piahs-375-19-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/piahs-375-19-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
Articles | Volume 375
03 Mar 2017
 | 03 Mar 2017

Modelling suspended sediment distribution in the Selenga River Delta using LandSat data

Sergey R. Chalov, Varvara O. Bazilova, and Mikhail K. Tarasov

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Cited articles

Chalov, S., Jarsjö, J., Kasimov, N., Romanchenko, A., Pietron, J., Thorslund, J., and Belozerova, E.: Spatio-temporal variation of sediment transport in the Selenga River Basin, Mongolia and Russia, Environ. Earth Sci., 73, 663–680, 2015.
Chalov, S., Thorslund, J., Kasimov, N. S., Nittrouer, J., Iliyecheva, E., Pavlov, M., Pietron, J., Shinkareva, G., Lychagin, M., Aybullatov, D., Kositsky, A., Tarasov, M., Akhtman, Y., Garmaev, E., Karthe, D., and Jarsjö, J.: The Selenga River delta: a geochemical barrier protecting Lake Baikal waters, Reg. Environ. Change, https://doi.org/10.1007/s10113-016-0996-1, in press, 2016.
Chalov, S. R. and Alexeevsky, N. I.: Braided rivers: structure, types and hydrological effects, Hydrol. Res., 46, 258–275, 2015.
Chalov, S. R., Kasimov, N. S., Lychagin, M. Y., Alekseevsky, N. I., Belozerova, E. V., Theuring, P., Shinkareva, G. L., Romanchenko, A. O., and Garmaev, E. J.: Water resources assessment of the Selenga–Baikal river system, GeoÖko, 34, 77–102, 2013.
Chavez, P. S.: Image-based atmospheric corrections-revisited and improved, Photogramm. Eng. Rem. S., 62, 1025–1035, 1996.
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The Selenga River is the largest tributary of Baikal Lake, it's delta covers around 600 km2. Suspended sediment concentrations (SSC) in the Selenga river delta were modelled based on LandSat images data. The variability in suspended sediment retention during the period 1989 to 2015 was calculated. The results suggest that SSC storage in the delta is observed during high discharges, whereas export increases under lower flow conditions. The changes in seasonal patterns are explained by wetland.
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