Deep ice-rich permafrost: Final report of the Yedoma Action Group
Permafrost landscapes are threatened by climate warming and degrade in different ways. This includes near surface processes such as active layer deepening, as well as extensive processes like thermal erosion, and development of thermokarst features. In the Siberian and North American late Pleistocen...
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International Permafrost Association
2017
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Online Access: | https://epic.awi.de/id/eprint/46674/ https://epic.awi.de/id/eprint/46674/1/Strauss_2017_FrozenGround_41_page_9.pdf https://ipa.arcticportal.org/images/fg/FrozenGround_41.pdf https://hdl.handle.net/10013/epic.daa0d281-f5f3-4d17-ae95-aec4283363e8 https://hdl.handle.net/ |
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ftawi:oai:epic.awi.de:46674 2023-05-15T16:36:39+02:00 Deep ice-rich permafrost: Final report of the Yedoma Action Group Strauss, Jens 2017 application/pdf https://epic.awi.de/id/eprint/46674/ https://epic.awi.de/id/eprint/46674/1/Strauss_2017_FrozenGround_41_page_9.pdf https://ipa.arcticportal.org/images/fg/FrozenGround_41.pdf https://hdl.handle.net/10013/epic.daa0d281-f5f3-4d17-ae95-aec4283363e8 https://hdl.handle.net/ unknown International Permafrost Association https://epic.awi.de/id/eprint/46674/1/Strauss_2017_FrozenGround_41_page_9.pdf https://hdl.handle.net/ Strauss, J. orcid:0000-0003-4678-4982 (2017) Deep ice-rich permafrost: Final report of the Yedoma Action Group , [Miscellaneous] hdl:10013/epic.daa0d281-f5f3-4d17-ae95-aec4283363e8 EPIC3Frozen Ground, International Permafrost Association, 41 Miscellaneous notRev 2017 ftawi 2021-12-24T15:43:41Z Permafrost landscapes are threatened by climate warming and degrade in different ways. This includes near surface processes such as active layer deepening, as well as extensive processes like thermal erosion, and development of thermokarst features. In the Siberian and North American late Pleistocene ice-rich yedoma, permafrost thaw processes cause surface subsidence of several tens of metres due to loss of ground ice. With thawing, currently freeze-locked organic matter can be mobilized and contribute to the carbon-climate feedback, which is a process of global significance if formerly inactive, fossil carbon is re-introduced into the active carbon cycle. Other/Unknown Material Ice permafrost Thermokarst Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
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Open Polar |
collection |
Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
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ftawi |
language |
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description |
Permafrost landscapes are threatened by climate warming and degrade in different ways. This includes near surface processes such as active layer deepening, as well as extensive processes like thermal erosion, and development of thermokarst features. In the Siberian and North American late Pleistocene ice-rich yedoma, permafrost thaw processes cause surface subsidence of several tens of metres due to loss of ground ice. With thawing, currently freeze-locked organic matter can be mobilized and contribute to the carbon-climate feedback, which is a process of global significance if formerly inactive, fossil carbon is re-introduced into the active carbon cycle. |
format |
Other/Unknown Material |
author |
Strauss, Jens |
spellingShingle |
Strauss, Jens Deep ice-rich permafrost: Final report of the Yedoma Action Group |
author_facet |
Strauss, Jens |
author_sort |
Strauss, Jens |
title |
Deep ice-rich permafrost: Final report of the Yedoma Action Group |
title_short |
Deep ice-rich permafrost: Final report of the Yedoma Action Group |
title_full |
Deep ice-rich permafrost: Final report of the Yedoma Action Group |
title_fullStr |
Deep ice-rich permafrost: Final report of the Yedoma Action Group |
title_full_unstemmed |
Deep ice-rich permafrost: Final report of the Yedoma Action Group |
title_sort |
deep ice-rich permafrost: final report of the yedoma action group |
publisher |
International Permafrost Association |
publishDate |
2017 |
url |
https://epic.awi.de/id/eprint/46674/ https://epic.awi.de/id/eprint/46674/1/Strauss_2017_FrozenGround_41_page_9.pdf https://ipa.arcticportal.org/images/fg/FrozenGround_41.pdf https://hdl.handle.net/10013/epic.daa0d281-f5f3-4d17-ae95-aec4283363e8 https://hdl.handle.net/ |
genre |
Ice permafrost Thermokarst |
genre_facet |
Ice permafrost Thermokarst |
op_source |
EPIC3Frozen Ground, International Permafrost Association, 41 |
op_relation |
https://epic.awi.de/id/eprint/46674/1/Strauss_2017_FrozenGround_41_page_9.pdf https://hdl.handle.net/ Strauss, J. orcid:0000-0003-4678-4982 (2017) Deep ice-rich permafrost: Final report of the Yedoma Action Group , [Miscellaneous] hdl:10013/epic.daa0d281-f5f3-4d17-ae95-aec4283363e8 |
_version_ |
1766026985641869312 |