Organic carbon in ice-rich permafrost
Permafrost, defined as ground that is frozen for at least two consecutive years, is a distinct feature of the terrestrial unglaciated Arctic. It covers approximately one quarter of the land area of the Northern Hemisphere (23,000,000 km²). Arctic landscapes, especially those underlain by permafrost,...
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ftubpotsdam:oai:kobv.de-opus4-uni-potsdam:7523 2024-05-19T07:35:37+00:00 Organic carbon in ice-rich permafrost Organischer Kohlenstoff in eisreichen Permafrostablagerungen Strauß, Jens 2015-04-15 application/pdf https://publishup.uni-potsdam.de/frontdoor/index/index/docId/7523 https://nbn-resolving.org/urn:nbn:de:kobv:517-opus4-75236 https://doi.org/10.25932/publishup-7523 https://publishup.uni-potsdam.de/files/7523/strauss_diss.pdf eng eng https://publishup.uni-potsdam.de/frontdoor/index/index/docId/7523 urn:nbn:de:kobv:517-opus4-75236 https://nbn-resolving.org/urn:nbn:de:kobv:517-opus4-75236 https://doi.org/10.25932/publishup-7523 https://publishup.uni-potsdam.de/files/7523/strauss_diss.pdf https://rightsstatements.org/vocab/InC/1.0/ info:eu-repo/semantics/openAccess ddc:550 Institut für Umweltwissenschaften und Geographie doctoralthesis doc-type:doctoralThesis 2015 ftubpotsdam https://doi.org/10.25932/publishup-7523 2024-04-30T23:32:08Z Permafrost, defined as ground that is frozen for at least two consecutive years, is a distinct feature of the terrestrial unglaciated Arctic. It covers approximately one quarter of the land area of the Northern Hemisphere (23,000,000 km²). Arctic landscapes, especially those underlain by permafrost, are threatened by climate warming and may degrade in different ways, including active layer deepening, thermal erosion, and development of rapid thaw features. In Siberian and Alaskan late Pleistocene ice-rich Yedoma permafrost, rapid and deep thaw processes (called thermokarst) can mobilize deep organic carbon (below 3 m depth) by surface subsidence due to loss of ground ice. Increased permafrost thaw could cause a feedback loop of global significance if its stored frozen organic carbon is reintroduced into the active carbon cycle as greenhouse gases, which accelerate warming and inducing more permafrost thaw and carbon release. To assess this concern, the major objective of the thesis was to enhance the understanding of the origin of Yedoma as well as to assess the associated organic carbon pool size and carbon quality (concerning degradability). The key research questions were: - How did Yedoma deposits accumulate? - How much organic carbon is stored in the Yedoma region? - What is the susceptibility of the Yedoma region's carbon for future decomposition? To address these three research questions, an interdisciplinary approach, including detailed field studies and sampling in Siberia and Alaska as well as methods of sedimentology, organic biogeochemistry, remote sensing, statistical analyses, and computational modeling were applied. To provide a panarctic context, this thesis additionally includes results both from a newly compiled northern circumpolar carbon database and from a model assessment of carbon fluxes in a warming Arctic. The Yedoma samples show a homogeneous grain-size composition. All samples were poorly sorted with a multi-modal grain-size distribution, indicating various (re-) transport processes. ... Doctoral or Postdoctoral Thesis Arctic Ice permafrost Thermokarst Alaska Siberia University of Potsdam: publish.UP |
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Open Polar |
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University of Potsdam: publish.UP |
op_collection_id |
ftubpotsdam |
language |
English |
topic |
ddc:550 Institut für Umweltwissenschaften und Geographie |
spellingShingle |
ddc:550 Institut für Umweltwissenschaften und Geographie Strauß, Jens Organic carbon in ice-rich permafrost |
topic_facet |
ddc:550 Institut für Umweltwissenschaften und Geographie |
description |
Permafrost, defined as ground that is frozen for at least two consecutive years, is a distinct feature of the terrestrial unglaciated Arctic. It covers approximately one quarter of the land area of the Northern Hemisphere (23,000,000 km²). Arctic landscapes, especially those underlain by permafrost, are threatened by climate warming and may degrade in different ways, including active layer deepening, thermal erosion, and development of rapid thaw features. In Siberian and Alaskan late Pleistocene ice-rich Yedoma permafrost, rapid and deep thaw processes (called thermokarst) can mobilize deep organic carbon (below 3 m depth) by surface subsidence due to loss of ground ice. Increased permafrost thaw could cause a feedback loop of global significance if its stored frozen organic carbon is reintroduced into the active carbon cycle as greenhouse gases, which accelerate warming and inducing more permafrost thaw and carbon release. To assess this concern, the major objective of the thesis was to enhance the understanding of the origin of Yedoma as well as to assess the associated organic carbon pool size and carbon quality (concerning degradability). The key research questions were: - How did Yedoma deposits accumulate? - How much organic carbon is stored in the Yedoma region? - What is the susceptibility of the Yedoma region's carbon for future decomposition? To address these three research questions, an interdisciplinary approach, including detailed field studies and sampling in Siberia and Alaska as well as methods of sedimentology, organic biogeochemistry, remote sensing, statistical analyses, and computational modeling were applied. To provide a panarctic context, this thesis additionally includes results both from a newly compiled northern circumpolar carbon database and from a model assessment of carbon fluxes in a warming Arctic. The Yedoma samples show a homogeneous grain-size composition. All samples were poorly sorted with a multi-modal grain-size distribution, indicating various (re-) transport processes. ... |
format |
Doctoral or Postdoctoral Thesis |
author |
Strauß, Jens |
author_facet |
Strauß, Jens |
author_sort |
Strauß, Jens |
title |
Organic carbon in ice-rich permafrost |
title_short |
Organic carbon in ice-rich permafrost |
title_full |
Organic carbon in ice-rich permafrost |
title_fullStr |
Organic carbon in ice-rich permafrost |
title_full_unstemmed |
Organic carbon in ice-rich permafrost |
title_sort |
organic carbon in ice-rich permafrost |
publishDate |
2015 |
url |
https://publishup.uni-potsdam.de/frontdoor/index/index/docId/7523 https://nbn-resolving.org/urn:nbn:de:kobv:517-opus4-75236 https://doi.org/10.25932/publishup-7523 https://publishup.uni-potsdam.de/files/7523/strauss_diss.pdf |
genre |
Arctic Ice permafrost Thermokarst Alaska Siberia |
genre_facet |
Arctic Ice permafrost Thermokarst Alaska Siberia |
op_relation |
https://publishup.uni-potsdam.de/frontdoor/index/index/docId/7523 urn:nbn:de:kobv:517-opus4-75236 https://nbn-resolving.org/urn:nbn:de:kobv:517-opus4-75236 https://doi.org/10.25932/publishup-7523 https://publishup.uni-potsdam.de/files/7523/strauss_diss.pdf |
op_rights |
https://rightsstatements.org/vocab/InC/1.0/ info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.25932/publishup-7523 |
_version_ |
1799474397619159040 |