Organic carbon – how much is stored in ice-rich permafrost?
Rapid changes are observed in the Polar Regions. With ongoing climate change, the Arctic will continue to warm approximately twice as fast as the lower latitudes. Vast areas of the Arctic are affected by permafrost where degradation processes such as thermokarst and thermal erosion are expected to i...
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ftawi:oai:epic.awi.de:50297 2023-05-15T14:55:07+02:00 Organic carbon – how much is stored in ice-rich permafrost? Jongejans, Loeka L. Strauss, Jens Mangelsdorf, Kai Lenz, Josefine Grosse, Guido 2019-09-10 https://epic.awi.de/id/eprint/50297/ https://hdl.handle.net/10013/epic.f1941229-f1e7-43c8-95da-c34cbea68466 unknown Jongejans, L. L. orcid:0000-0002-0383-4567 , Strauss, J. orcid:0000-0003-4678-4982 , Mangelsdorf, K. orcid:0000-0003-3283-3448 , Lenz, J. orcid:0000-0002-4050-3169 and Grosse, G. orcid:0000-0001-5895-2141 (2019) Organic carbon – how much is stored in ice-rich permafrost? , YES Congress 2019, Freie Universität Berlin, 9 September 2019 - 13 September 2019 . hdl:10013/epic.f1941229-f1e7-43c8-95da-c34cbea68466 EPIC3YES Congress 2019, Freie Universität Berlin, 2019-09-09-2019-09-13 Conference notRev 2019 ftawi 2021-12-24T15:44:58Z Rapid changes are observed in the Polar Regions. With ongoing climate change, the Arctic will continue to warm approximately twice as fast as the lower latitudes. Vast areas of the Arctic are affected by permafrost where degradation processes such as thermokarst and thermal erosion are expected to increase considerably. Large areas in Alaska and Siberia are covered by ice-rich permafrost, such as yedoma permafrost. These deposits reach a thickness up to 50 m and include large ice-wedges. Thus, warming can trigger deep thaw processes which can mobilize organic carbon well below 1 m soil depth. Consequently, permafrost carbon storage is becoming increasingly vulnerable with ongoing permafrost thaw. Undisturbed yedoma deposits are characterized by relatively high quality organic carbon stored and are presumably highly susceptible for future degradation. We aim to identify the quantity and quality of the organic matter, in order to improve the estimates of the rate and amount of organic carbon that can be released from permafrost thaw with warming. Conference Object Arctic Climate change Ice permafrost Thermokarst wedge* Alaska Siberia Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) Arctic |
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Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
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ftawi |
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description |
Rapid changes are observed in the Polar Regions. With ongoing climate change, the Arctic will continue to warm approximately twice as fast as the lower latitudes. Vast areas of the Arctic are affected by permafrost where degradation processes such as thermokarst and thermal erosion are expected to increase considerably. Large areas in Alaska and Siberia are covered by ice-rich permafrost, such as yedoma permafrost. These deposits reach a thickness up to 50 m and include large ice-wedges. Thus, warming can trigger deep thaw processes which can mobilize organic carbon well below 1 m soil depth. Consequently, permafrost carbon storage is becoming increasingly vulnerable with ongoing permafrost thaw. Undisturbed yedoma deposits are characterized by relatively high quality organic carbon stored and are presumably highly susceptible for future degradation. We aim to identify the quantity and quality of the organic matter, in order to improve the estimates of the rate and amount of organic carbon that can be released from permafrost thaw with warming. |
format |
Conference Object |
author |
Jongejans, Loeka L. Strauss, Jens Mangelsdorf, Kai Lenz, Josefine Grosse, Guido |
spellingShingle |
Jongejans, Loeka L. Strauss, Jens Mangelsdorf, Kai Lenz, Josefine Grosse, Guido Organic carbon – how much is stored in ice-rich permafrost? |
author_facet |
Jongejans, Loeka L. Strauss, Jens Mangelsdorf, Kai Lenz, Josefine Grosse, Guido |
author_sort |
Jongejans, Loeka L. |
title |
Organic carbon – how much is stored in ice-rich permafrost? |
title_short |
Organic carbon – how much is stored in ice-rich permafrost? |
title_full |
Organic carbon – how much is stored in ice-rich permafrost? |
title_fullStr |
Organic carbon – how much is stored in ice-rich permafrost? |
title_full_unstemmed |
Organic carbon – how much is stored in ice-rich permafrost? |
title_sort |
organic carbon – how much is stored in ice-rich permafrost? |
publishDate |
2019 |
url |
https://epic.awi.de/id/eprint/50297/ https://hdl.handle.net/10013/epic.f1941229-f1e7-43c8-95da-c34cbea68466 |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic Climate change Ice permafrost Thermokarst wedge* Alaska Siberia |
genre_facet |
Arctic Climate change Ice permafrost Thermokarst wedge* Alaska Siberia |
op_source |
EPIC3YES Congress 2019, Freie Universität Berlin, 2019-09-09-2019-09-13 |
op_relation |
Jongejans, L. L. orcid:0000-0002-0383-4567 , Strauss, J. orcid:0000-0003-4678-4982 , Mangelsdorf, K. orcid:0000-0003-3283-3448 , Lenz, J. orcid:0000-0002-4050-3169 and Grosse, G. orcid:0000-0001-5895-2141 (2019) Organic carbon – how much is stored in ice-rich permafrost? , YES Congress 2019, Freie Universität Berlin, 9 September 2019 - 13 September 2019 . hdl:10013/epic.f1941229-f1e7-43c8-95da-c34cbea68466 |
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1766326897095999488 |