Spatial and temporal variability of suspended sediment yield in the Kamchatka Krai, Russian Federation
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 river...
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ftnonlinearchiv:oai:noa.gwlb.de:cop_mods_00017388 2023-05-15T16:58:33+02:00 Spatial and temporal variability of suspended sediment yield in the Kamchatka Krai, Russian Federation Kuksina, L. Alexeevsky, N. 2015-03 electronic 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 eng eng Copernicus Publications Proceedings of the International Association of Hydrological Sciences -- https://www.proc-iahs.net/volumes.html -- http://www.bibliothek.uni-regensburg.de/ezeit/?2827925 -- 2199-899X 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 uneingeschränkt info:eu-repo/semantics/openAccess article Verlagsveröffentlichung article Text doc-type:article 2015 ftnonlinearchiv https://doi.org/10.5194/piahs-367-304-2015 2022-02-08T22:53:44Z 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. Article in Journal/Newspaper Kamchatka Niedersächsisches Online-Archiv NOA Kamchatka Krai ENVELOPE(159.000,159.000,55.000,55.000) Proceedings of the International Association of Hydrological Sciences 367 304 311 |
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Niedersächsisches Online-Archiv NOA |
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English |
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article Verlagsveröffentlichung |
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article Verlagsveröffentlichung Kuksina, L. Alexeevsky, N. Spatial and temporal variability of suspended sediment yield in the Kamchatka Krai, Russian Federation |
topic_facet |
article Verlagsveröffentlichung |
description |
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. |
format |
Article in Journal/Newspaper |
author |
Kuksina, L. Alexeevsky, N. |
author_facet |
Kuksina, L. Alexeevsky, N. |
author_sort |
Kuksina, L. |
title |
Spatial and temporal variability of suspended sediment yield in the Kamchatka Krai, Russian Federation |
title_short |
Spatial and temporal variability of suspended sediment yield in the Kamchatka Krai, Russian Federation |
title_full |
Spatial and temporal variability of suspended sediment yield in the Kamchatka Krai, Russian Federation |
title_fullStr |
Spatial and temporal variability of suspended sediment yield in the Kamchatka Krai, Russian Federation |
title_full_unstemmed |
Spatial and temporal variability of suspended sediment yield in the Kamchatka Krai, Russian Federation |
title_sort |
spatial and temporal variability of suspended sediment yield in the kamchatka krai, russian federation |
publisher |
Copernicus Publications |
publishDate |
2015 |
url |
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 |
long_lat |
ENVELOPE(159.000,159.000,55.000,55.000) |
geographic |
Kamchatka Krai |
geographic_facet |
Kamchatka Krai |
genre |
Kamchatka |
genre_facet |
Kamchatka |
op_relation |
Proceedings of the International Association of Hydrological Sciences -- https://www.proc-iahs.net/volumes.html -- http://www.bibliothek.uni-regensburg.de/ezeit/?2827925 -- 2199-899X 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 |
op_rights |
uneingeschränkt info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.5194/piahs-367-304-2015 |
container_title |
Proceedings of the International Association of Hydrological Sciences |
container_volume |
367 |
container_start_page |
304 |
op_container_end_page |
311 |
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1766050584817827840 |