Spatial and temporal variability of suspended sediment yield in the Kamchatka Krai, Russian Federation

• Published in: Proceedings of the International Association of Hydrological Sciences
• Main Authors: Kuksina, L., Alexeevsky, N.
• Format: Article in Journal/Newspaper
• Language: English
• Published: Copernicus Publications 2015
• Subjects: article; Verlagsveröffentlichung; Kamchatka Krai; Kamchatka
• Online Access: https://doi.org/10.5194/piahs-367-304-2015; https://noa.gwlb.de/receive/cop_mods_00017388; https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00017343/piahs-367-304-2015.pdf; https://piahs.copernicus.org/articles/367/304/2015/piahs-367-304-2015.pdf

Research into the spatial and temporal variability of suspended sediment flux (SSF, t year−1) has been conducted for rivers in the Kamchatka Krai (in the far east of the Russian Federation). The study of long-term fluctuations in SSF was based on difference-integral curve analysis. Most of the rivers in the region are characterized by two relatively long-term trends in SSF; increases from the late 1970s to the early 1980s, followed by a subsequent decline. Kamchatka was divided into regions based on similar conditions of specific suspended sediment yield (SSSY, t km−2 year−1) followed by a determination of the various factors controlling it. New maps of suspended sediment concentration (SSC, mg L−1) and SSSY for Kamchatka also were constructed and, based on this study, there currently appear to be 18 SSC and 13 SSSY regions, as opposed to 4 and 2 regions, respectively, as had been determined in the 1970s. The influence of volcanoes on SSF can be substantial, and can increase up to 5-fold after eruptions; SSC can reach 6∙105 mg L−1 in rivers draining the flanks of volcanoes.