First Quantification of the Permafrost Heat Sink in the Earth's Climate System ...

Due to an imbalance between incoming and outgoing radiation at the top of the atmosphere, excess heat has accumulated in Earth's climate system in recent decades, driving global warming and climatic changes. To date, it has not been quantified how much of this excess heat is used to melt ground...

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Main Authors: Nitzbon, Jan, Krinner, Gerhard, Schneider Von Deimling, Thomas, Werner, Martin, Langer, Moritz
Format: Text
Language:English
Published: Humboldt-Universität zu Berlin 2023
Subjects:
Ice
Online Access:https://dx.doi.org/10.18452/26963
https://edoc.hu-berlin.de/handle/18452/27651
id ftdatacite:10.18452/26963
record_format openpolar
spelling ftdatacite:10.18452/26963 2024-09-15T18:11:22+00:00 First Quantification of the Permafrost Heat Sink in the Earth's Climate System ... Nitzbon, Jan Krinner, Gerhard Schneider Von Deimling, Thomas Werner, Martin Langer, Moritz 2023 https://dx.doi.org/10.18452/26963 https://edoc.hu-berlin.de/handle/18452/27651 en eng Humboldt-Universität zu Berlin Creative Commons Attribution 4.0 International (CC BY 4.0) Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 permafrost Earth’s energy imbalance essential climate variable heat sink CryoGrid land surface model 550 Geowissenschaften Text article article-journal ScholarlyArticle 2023 ftdatacite https://doi.org/10.18452/26963 2024-09-02T08:58:24Z Due to an imbalance between incoming and outgoing radiation at the top of the atmosphere, excess heat has accumulated in Earth's climate system in recent decades, driving global warming and climatic changes. To date, it has not been quantified how much of this excess heat is used to melt ground ice in permafrost. Here, we diagnose changes in sensible and latent ground heat contents in the northern terrestrial permafrost region from ensemble-simulations of a tailored land surface model. We find that between 1980 and 2018, about 3.9^+1.4_-1.6 ZJ of heat, of which 1.7_-1.4^+1.3 ZJ (44%) were used to melt ground ice, were absorbed by permafrost. Our estimate, which does not yet account for the potentially increased heat uptake due to thermokarst processes in ice-rich terrain, suggests that permafrost is a persistent heat sink comparable in magnitude to other components of the cryosphere and must be explicitly considered when assessing Earth's energy imbalance. ... Text Ice permafrost Thermokarst DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic permafrost
Earth’s energy imbalance
essential climate variable
heat sink
CryoGrid
land surface model
550 Geowissenschaften
spellingShingle permafrost
Earth’s energy imbalance
essential climate variable
heat sink
CryoGrid
land surface model
550 Geowissenschaften
Nitzbon, Jan
Krinner, Gerhard
Schneider Von Deimling, Thomas
Werner, Martin
Langer, Moritz
First Quantification of the Permafrost Heat Sink in the Earth's Climate System ...
topic_facet permafrost
Earth’s energy imbalance
essential climate variable
heat sink
CryoGrid
land surface model
550 Geowissenschaften
description Due to an imbalance between incoming and outgoing radiation at the top of the atmosphere, excess heat has accumulated in Earth's climate system in recent decades, driving global warming and climatic changes. To date, it has not been quantified how much of this excess heat is used to melt ground ice in permafrost. Here, we diagnose changes in sensible and latent ground heat contents in the northern terrestrial permafrost region from ensemble-simulations of a tailored land surface model. We find that between 1980 and 2018, about 3.9^+1.4_-1.6 ZJ of heat, of which 1.7_-1.4^+1.3 ZJ (44%) were used to melt ground ice, were absorbed by permafrost. Our estimate, which does not yet account for the potentially increased heat uptake due to thermokarst processes in ice-rich terrain, suggests that permafrost is a persistent heat sink comparable in magnitude to other components of the cryosphere and must be explicitly considered when assessing Earth's energy imbalance. ...
format Text
author Nitzbon, Jan
Krinner, Gerhard
Schneider Von Deimling, Thomas
Werner, Martin
Langer, Moritz
author_facet Nitzbon, Jan
Krinner, Gerhard
Schneider Von Deimling, Thomas
Werner, Martin
Langer, Moritz
author_sort Nitzbon, Jan
title First Quantification of the Permafrost Heat Sink in the Earth's Climate System ...
title_short First Quantification of the Permafrost Heat Sink in the Earth's Climate System ...
title_full First Quantification of the Permafrost Heat Sink in the Earth's Climate System ...
title_fullStr First Quantification of the Permafrost Heat Sink in the Earth's Climate System ...
title_full_unstemmed First Quantification of the Permafrost Heat Sink in the Earth's Climate System ...
title_sort first quantification of the permafrost heat sink in the earth's climate system ...
publisher Humboldt-Universität zu Berlin
publishDate 2023
url https://dx.doi.org/10.18452/26963
https://edoc.hu-berlin.de/handle/18452/27651
genre Ice
permafrost
Thermokarst
genre_facet Ice
permafrost
Thermokarst
op_rights Creative Commons Attribution 4.0 International
(CC BY 4.0) Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_doi https://doi.org/10.18452/26963
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