Amplified carbon release from vast West Siberian peatlands by 2100
Extensive new data from previously unstudied Siberian streams and rivers suggest that mobilization of currently frozen, high-latitude soil carbon is likely over the next century in response to predicted Arctic warming. We present dissolved organic carbon (DOC) measurements from ninety-six watersheds...
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ftclarkuniv:oai:commons.clarku.edu:faculty_geography-1248 2023-09-05T13:16:37+02:00 Amplified carbon release from vast West Siberian peatlands by 2100 Frey, Karen E. Smith, Laurence C. 2005-05-16T07:00:00Z application/pdf https://commons.clarku.edu/faculty_geography/249 https://doi.org/10.1029/2004GL022025 https://commons.clarku.edu/context/faculty_geography/article/1248/viewcontent/GeogFacWorks_Frey_Amplifiedcarbon_2005.pdf unknown Clark Digital Commons https://commons.clarku.edu/faculty_geography/249 doi:10.1029/2004GL022025 https://commons.clarku.edu/context/faculty_geography/article/1248/viewcontent/GeogFacWorks_Frey_Amplifiedcarbon_2005.pdf Geography Siberia permafrost carbon Arctic Ocean Geography Social and Behavioral Sciences text 2005 ftclarkuniv https://doi.org/10.1029/2004GL022025 2023-08-14T06:16:31Z Extensive new data from previously unstudied Siberian streams and rivers suggest that mobilization of currently frozen, high-latitude soil carbon is likely over the next century in response to predicted Arctic warming. We present dissolved organic carbon (DOC) measurements from ninety-six watersheds in West Siberia, a region that contains the world's largest stores of peat carbon, exports massive volumes of freshwater and DOC to the Arctic Ocean, and is warming faster than the Arctic as a whole. The sample sites span ∼106 km2 over a large climatic gradient (∼55-68°N), providing data on a much broader spatial scale than previous studies and for the first time explicitly examining stream DOC in permafrost peatland environments. Our results show that cold, permafrost-influenced watersheds release little DOC to streams, regardless of the extent of peatland cover. However, we find considerably higher concentrations in warm, permafrost-free watersheds, rising sharply as a function of peatland cover. The two regimes are demarcated by the position of the -2°C mean annual air temperature (MAAT) isotherm, which is also approximately coincident with the permafrost limit. Climate model simulations for the next century predict near-doubling of West Siberian land surface areas with a MAAT warmer than -2°C, suggesting up to ∼700% increases in stream DOC concentrations and ∼2.7-4.3 Tg yr-1 (∼29-46%) increases in DOC flux to the Arctic Ocean. Copyright 2005 by the American Geophysical Union. Text Arctic Arctic Ocean permafrost Siberia Clark University: Clark Digital Commons Arctic Arctic Ocean Geophysical Research Letters 32 9 |
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Open Polar |
collection |
Clark University: Clark Digital Commons |
op_collection_id |
ftclarkuniv |
language |
unknown |
topic |
Siberia permafrost carbon Arctic Ocean Geography Social and Behavioral Sciences |
spellingShingle |
Siberia permafrost carbon Arctic Ocean Geography Social and Behavioral Sciences Frey, Karen E. Smith, Laurence C. Amplified carbon release from vast West Siberian peatlands by 2100 |
topic_facet |
Siberia permafrost carbon Arctic Ocean Geography Social and Behavioral Sciences |
description |
Extensive new data from previously unstudied Siberian streams and rivers suggest that mobilization of currently frozen, high-latitude soil carbon is likely over the next century in response to predicted Arctic warming. We present dissolved organic carbon (DOC) measurements from ninety-six watersheds in West Siberia, a region that contains the world's largest stores of peat carbon, exports massive volumes of freshwater and DOC to the Arctic Ocean, and is warming faster than the Arctic as a whole. The sample sites span ∼106 km2 over a large climatic gradient (∼55-68°N), providing data on a much broader spatial scale than previous studies and for the first time explicitly examining stream DOC in permafrost peatland environments. Our results show that cold, permafrost-influenced watersheds release little DOC to streams, regardless of the extent of peatland cover. However, we find considerably higher concentrations in warm, permafrost-free watersheds, rising sharply as a function of peatland cover. The two regimes are demarcated by the position of the -2°C mean annual air temperature (MAAT) isotherm, which is also approximately coincident with the permafrost limit. Climate model simulations for the next century predict near-doubling of West Siberian land surface areas with a MAAT warmer than -2°C, suggesting up to ∼700% increases in stream DOC concentrations and ∼2.7-4.3 Tg yr-1 (∼29-46%) increases in DOC flux to the Arctic Ocean. Copyright 2005 by the American Geophysical Union. |
format |
Text |
author |
Frey, Karen E. Smith, Laurence C. |
author_facet |
Frey, Karen E. Smith, Laurence C. |
author_sort |
Frey, Karen E. |
title |
Amplified carbon release from vast West Siberian peatlands by 2100 |
title_short |
Amplified carbon release from vast West Siberian peatlands by 2100 |
title_full |
Amplified carbon release from vast West Siberian peatlands by 2100 |
title_fullStr |
Amplified carbon release from vast West Siberian peatlands by 2100 |
title_full_unstemmed |
Amplified carbon release from vast West Siberian peatlands by 2100 |
title_sort |
amplified carbon release from vast west siberian peatlands by 2100 |
publisher |
Clark Digital Commons |
publishDate |
2005 |
url |
https://commons.clarku.edu/faculty_geography/249 https://doi.org/10.1029/2004GL022025 https://commons.clarku.edu/context/faculty_geography/article/1248/viewcontent/GeogFacWorks_Frey_Amplifiedcarbon_2005.pdf |
geographic |
Arctic Arctic Ocean |
geographic_facet |
Arctic Arctic Ocean |
genre |
Arctic Arctic Ocean permafrost Siberia |
genre_facet |
Arctic Arctic Ocean permafrost Siberia |
op_source |
Geography |
op_relation |
https://commons.clarku.edu/faculty_geography/249 doi:10.1029/2004GL022025 https://commons.clarku.edu/context/faculty_geography/article/1248/viewcontent/GeogFacWorks_Frey_Amplifiedcarbon_2005.pdf |
op_doi |
https://doi.org/10.1029/2004GL022025 |
container_title |
Geophysical Research Letters |
container_volume |
32 |
container_issue |
9 |
_version_ |
1776198133392343040 |