Hydroclimatic anomalies detected by a sub-decadal diatom oxygen isotope record of the last 220 years from Lake Khamra, Siberia
Northern latitudes have been significantly impacted by recent climate warming, which has increased the probability of experiencing extreme weather events. To comprehensively understand hydroclimate change and reconstruct hydroclimatic anomalies such as drought periods, appropriate proxy records reac...
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ftcopernicus:oai:publications.copernicus.org:cp115523 2024-09-15T18:02:36+00:00 Hydroclimatic anomalies detected by a sub-decadal diatom oxygen isotope record of the last 220 years from Lake Khamra, Siberia Stieg, Amelie Biskaborn, Boris K. Herzschuh, Ulrike Strauss, Jens Pestryakova, Luidmila Meyer, Hanno 2024-04-11 application/pdf https://doi.org/10.5194/cp-20-909-2024 https://cp.copernicus.org/articles/20/909/2024/ eng eng doi:10.5194/cp-20-909-2024 https://cp.copernicus.org/articles/20/909/2024/ eISSN: 1814-9332 Text 2024 ftcopernicus https://doi.org/10.5194/cp-20-909-2024 2024-08-28T05:24:15Z Northern latitudes have been significantly impacted by recent climate warming, which has increased the probability of experiencing extreme weather events. To comprehensively understand hydroclimate change and reconstruct hydroclimatic anomalies such as drought periods, appropriate proxy records reaching further back in time beyond meteorological measurements are needed. Here we present a 220-year (2015–1790 CE), continuous, stable oxygen isotope record of diatoms ( δ 18 O diatom ) from Lake Khamra (59.99° N, 112.98° E) in eastern Siberia, an area highly sensitive to climate change and for which there is a demand for palaeohydrological data. This high-resolution proxy record was obtained from a 210 Pb– 137 Cs-dated sediment short core and analysed to reconstruct hydroclimate variability at a sub-decadal scale. The interpretation of the δ 18 O diatom record is supported by meteorological data, modern isotope hydrology and geochemical analyses of the same sediment, which is indicative of the conditions in the lake and catchment. A comparison with meteorological data going back to 1930 CE revealed that the δ 18 O diatom record of Lake Khamra is primarily influenced by regional precipitation changes rather than the air temperature. We identified winter precipitation, which enters the lake as isotopically depleted snowmelt water, as the key process impacting the diatom isotope variability. We related the overall depletion of δ 18 O diatom in recent decades to an observed increase in winter precipitation in the area, likely associated with the global air temperature rise, Arctic sea ice retreat and increased moisture transport inland. Available palaeoclimate proxy records, including a fire reconstruction for the same lake, support the idea that the new record is a valuable hydroclimate proxy that is indicative of precipitation deficits and excludes solar insolation and air temperature as primary driving forces, even before the first meteorological recordings. We propose two possible hydroclimatic anomalies that were ... Text Climate change Sea ice Siberia Copernicus Publications: E-Journals Climate of the Past 20 4 909 933 |
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English |
description |
Northern latitudes have been significantly impacted by recent climate warming, which has increased the probability of experiencing extreme weather events. To comprehensively understand hydroclimate change and reconstruct hydroclimatic anomalies such as drought periods, appropriate proxy records reaching further back in time beyond meteorological measurements are needed. Here we present a 220-year (2015–1790 CE), continuous, stable oxygen isotope record of diatoms ( δ 18 O diatom ) from Lake Khamra (59.99° N, 112.98° E) in eastern Siberia, an area highly sensitive to climate change and for which there is a demand for palaeohydrological data. This high-resolution proxy record was obtained from a 210 Pb– 137 Cs-dated sediment short core and analysed to reconstruct hydroclimate variability at a sub-decadal scale. The interpretation of the δ 18 O diatom record is supported by meteorological data, modern isotope hydrology and geochemical analyses of the same sediment, which is indicative of the conditions in the lake and catchment. A comparison with meteorological data going back to 1930 CE revealed that the δ 18 O diatom record of Lake Khamra is primarily influenced by regional precipitation changes rather than the air temperature. We identified winter precipitation, which enters the lake as isotopically depleted snowmelt water, as the key process impacting the diatom isotope variability. We related the overall depletion of δ 18 O diatom in recent decades to an observed increase in winter precipitation in the area, likely associated with the global air temperature rise, Arctic sea ice retreat and increased moisture transport inland. Available palaeoclimate proxy records, including a fire reconstruction for the same lake, support the idea that the new record is a valuable hydroclimate proxy that is indicative of precipitation deficits and excludes solar insolation and air temperature as primary driving forces, even before the first meteorological recordings. We propose two possible hydroclimatic anomalies that were ... |
format |
Text |
author |
Stieg, Amelie Biskaborn, Boris K. Herzschuh, Ulrike Strauss, Jens Pestryakova, Luidmila Meyer, Hanno |
spellingShingle |
Stieg, Amelie Biskaborn, Boris K. Herzschuh, Ulrike Strauss, Jens Pestryakova, Luidmila Meyer, Hanno Hydroclimatic anomalies detected by a sub-decadal diatom oxygen isotope record of the last 220 years from Lake Khamra, Siberia |
author_facet |
Stieg, Amelie Biskaborn, Boris K. Herzschuh, Ulrike Strauss, Jens Pestryakova, Luidmila Meyer, Hanno |
author_sort |
Stieg, Amelie |
title |
Hydroclimatic anomalies detected by a sub-decadal diatom oxygen isotope record of the last 220 years from Lake Khamra, Siberia |
title_short |
Hydroclimatic anomalies detected by a sub-decadal diatom oxygen isotope record of the last 220 years from Lake Khamra, Siberia |
title_full |
Hydroclimatic anomalies detected by a sub-decadal diatom oxygen isotope record of the last 220 years from Lake Khamra, Siberia |
title_fullStr |
Hydroclimatic anomalies detected by a sub-decadal diatom oxygen isotope record of the last 220 years from Lake Khamra, Siberia |
title_full_unstemmed |
Hydroclimatic anomalies detected by a sub-decadal diatom oxygen isotope record of the last 220 years from Lake Khamra, Siberia |
title_sort |
hydroclimatic anomalies detected by a sub-decadal diatom oxygen isotope record of the last 220 years from lake khamra, siberia |
publishDate |
2024 |
url |
https://doi.org/10.5194/cp-20-909-2024 https://cp.copernicus.org/articles/20/909/2024/ |
genre |
Climate change Sea ice Siberia |
genre_facet |
Climate change Sea ice Siberia |
op_source |
eISSN: 1814-9332 |
op_relation |
doi:10.5194/cp-20-909-2024 https://cp.copernicus.org/articles/20/909/2024/ |
op_doi |
https://doi.org/10.5194/cp-20-909-2024 |
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Climate of the Past |
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