Complex streamflow responses to climate warming in five river basins in South Yakutia, Russia
The climate is warming much faster than the global average at the northern mid–high latitudes, leading to intensified hydrological cycles. However, it is unclear whether the response of streamflow to climate change is uniform across river basins with areas of 104–105 km2. In this study, monthly stre...
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Online Access: | https://doi.org/10.3389/fenvs.2022.1033943 https://doaj.org/article/46f4335c83724044b746923252fa0179 |
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fttriple:oai:gotriple.eu:oai:doaj.org/article:46f4335c83724044b746923252fa0179 2023-05-15T17:57:27+02:00 Complex streamflow responses to climate warming in five river basins in South Yakutia, Russia Ping Wang Raisa N. Shpakova 2022-10-01 https://doi.org/10.3389/fenvs.2022.1033943 https://doaj.org/article/46f4335c83724044b746923252fa0179 en eng Frontiers Media S.A. 2296-665X doi:10.3389/fenvs.2022.1033943 https://doaj.org/article/46f4335c83724044b746923252fa0179 undefined Frontiers in Environmental Science, Vol 10 (2022) streamflow climate warming permafrost degradation Siberia precipitation envir geo Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2022 fttriple https://doi.org/10.3389/fenvs.2022.1033943 2023-01-22T19:33:18Z The climate is warming much faster than the global average at the northern mid–high latitudes, leading to intensified hydrological cycles. However, it is unclear whether the response of streamflow to climate change is uniform across river basins with areas of 104–105 km2. In this study, monthly streamflow data from five river basins (Bol’shoy Patom, Chara, Olekma, Timpton, and Uchur) and gridded monthly temperature and precipitation data from the Russian South Yakutia at 53.5–61.5°N were analysed to investigate changes in their annual streamflow from 1934 to 2019 and their responses to climate warming. The results showed significant increasing trends in air temperature for all five basins at rates of 0.20°C–0.22°C/decade (p 0.05). By analysing the temperature-precipitation-streamflow relationships, we determined that the annual streamflow positively responds to precipitation, while winter streamflow is most sensitive to temperature. With climate warming, the streamflow during the winter period (October-April) increased significantly in four of the five river basins at rates of 1.4–3.1 mm/decade (p < 0.001), suggesting that warming-induced permafrost thawing increases baseflow. Although the streamflow response of large Siberian rivers to climate change is consistent, our results suggest that the streamflow response to climate change in relatively small river basins (104–105 km2) is much more complex. Article in Journal/Newspaper permafrost Yakutia Siberia Unknown Frontiers in Environmental Science 10 |
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streamflow climate warming permafrost degradation Siberia precipitation envir geo |
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streamflow climate warming permafrost degradation Siberia precipitation envir geo Ping Wang Raisa N. Shpakova Complex streamflow responses to climate warming in five river basins in South Yakutia, Russia |
topic_facet |
streamflow climate warming permafrost degradation Siberia precipitation envir geo |
description |
The climate is warming much faster than the global average at the northern mid–high latitudes, leading to intensified hydrological cycles. However, it is unclear whether the response of streamflow to climate change is uniform across river basins with areas of 104–105 km2. In this study, monthly streamflow data from five river basins (Bol’shoy Patom, Chara, Olekma, Timpton, and Uchur) and gridded monthly temperature and precipitation data from the Russian South Yakutia at 53.5–61.5°N were analysed to investigate changes in their annual streamflow from 1934 to 2019 and their responses to climate warming. The results showed significant increasing trends in air temperature for all five basins at rates of 0.20°C–0.22°C/decade (p 0.05). By analysing the temperature-precipitation-streamflow relationships, we determined that the annual streamflow positively responds to precipitation, while winter streamflow is most sensitive to temperature. With climate warming, the streamflow during the winter period (October-April) increased significantly in four of the five river basins at rates of 1.4–3.1 mm/decade (p < 0.001), suggesting that warming-induced permafrost thawing increases baseflow. Although the streamflow response of large Siberian rivers to climate change is consistent, our results suggest that the streamflow response to climate change in relatively small river basins (104–105 km2) is much more complex. |
format |
Article in Journal/Newspaper |
author |
Ping Wang Raisa N. Shpakova |
author_facet |
Ping Wang Raisa N. Shpakova |
author_sort |
Ping Wang |
title |
Complex streamflow responses to climate warming in five river basins in South Yakutia, Russia |
title_short |
Complex streamflow responses to climate warming in five river basins in South Yakutia, Russia |
title_full |
Complex streamflow responses to climate warming in five river basins in South Yakutia, Russia |
title_fullStr |
Complex streamflow responses to climate warming in five river basins in South Yakutia, Russia |
title_full_unstemmed |
Complex streamflow responses to climate warming in five river basins in South Yakutia, Russia |
title_sort |
complex streamflow responses to climate warming in five river basins in south yakutia, russia |
publisher |
Frontiers Media S.A. |
publishDate |
2022 |
url |
https://doi.org/10.3389/fenvs.2022.1033943 https://doaj.org/article/46f4335c83724044b746923252fa0179 |
genre |
permafrost Yakutia Siberia |
genre_facet |
permafrost Yakutia Siberia |
op_source |
Frontiers in Environmental Science, Vol 10 (2022) |
op_relation |
2296-665X doi:10.3389/fenvs.2022.1033943 https://doaj.org/article/46f4335c83724044b746923252fa0179 |
op_rights |
undefined |
op_doi |
https://doi.org/10.3389/fenvs.2022.1033943 |
container_title |
Frontiers in Environmental Science |
container_volume |
10 |
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1766165881288654848 |