A simplified permafrost-carbon model for long-term climate studies with the CLIMBER-2 coupled earth system model
We present the development and validation of a simplified permafrost-carbon mechanism for use with the land surface scheme operating in the CLIMBER-2 earth system model. The simplified model estimates the permafrost fraction of each grid cell according to the balance between modelled cold (below 0 °...
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2014
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Online Access: | https://doi.org/10.5194/gmd-7-3111-2014 https://doaj.org/article/7c13e3287116480ca54d1502a9fe0119 |
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ftdoajarticles:oai:doaj.org/article:7c13e3287116480ca54d1502a9fe0119 2023-05-15T17:55:27+02:00 A simplified permafrost-carbon model for long-term climate studies with the CLIMBER-2 coupled earth system model K. A. Crichton D. M. Roche G. Krinner J. Chappellaz 2014-12-01T00:00:00Z https://doi.org/10.5194/gmd-7-3111-2014 https://doaj.org/article/7c13e3287116480ca54d1502a9fe0119 EN eng Copernicus Publications http://www.geosci-model-dev.net/7/3111/2014/gmd-7-3111-2014.pdf https://doaj.org/toc/1991-959X https://doaj.org/toc/1991-9603 1991-959X 1991-9603 doi:10.5194/gmd-7-3111-2014 https://doaj.org/article/7c13e3287116480ca54d1502a9fe0119 Geoscientific Model Development, Vol 7, Iss 6, Pp 3111-3134 (2014) Geology QE1-996.5 article 2014 ftdoajarticles https://doi.org/10.5194/gmd-7-3111-2014 2022-12-31T00:31:34Z We present the development and validation of a simplified permafrost-carbon mechanism for use with the land surface scheme operating in the CLIMBER-2 earth system model. The simplified model estimates the permafrost fraction of each grid cell according to the balance between modelled cold (below 0 °C) and warm (above 0 °C) days in a year. Areas diagnosed as permafrost are assigned a reduction in soil decomposition rate, thus creating a slow accumulating soil carbon pool. In warming climates, permafrost extent reduces and soil decomposition rates increase, resulting in soil carbon release to the atmosphere. Four accumulation/decomposition rate settings are retained for experiments within the CLIMBER-2(P) model, which are tuned to agree with estimates of total land carbon stocks today and at the last glacial maximum. The distribution of this permafrost-carbon pool is in broad agreement with measurement data for soil carbon content. The level of complexity of the permafrost-carbon model is comparable to other components in the CLIMBER-2 earth system model. Article in Journal/Newspaper permafrost Directory of Open Access Journals: DOAJ Articles Geoscientific Model Development 7 6 3111 3134 |
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Open Polar |
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Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Geology QE1-996.5 |
spellingShingle |
Geology QE1-996.5 K. A. Crichton D. M. Roche G. Krinner J. Chappellaz A simplified permafrost-carbon model for long-term climate studies with the CLIMBER-2 coupled earth system model |
topic_facet |
Geology QE1-996.5 |
description |
We present the development and validation of a simplified permafrost-carbon mechanism for use with the land surface scheme operating in the CLIMBER-2 earth system model. The simplified model estimates the permafrost fraction of each grid cell according to the balance between modelled cold (below 0 °C) and warm (above 0 °C) days in a year. Areas diagnosed as permafrost are assigned a reduction in soil decomposition rate, thus creating a slow accumulating soil carbon pool. In warming climates, permafrost extent reduces and soil decomposition rates increase, resulting in soil carbon release to the atmosphere. Four accumulation/decomposition rate settings are retained for experiments within the CLIMBER-2(P) model, which are tuned to agree with estimates of total land carbon stocks today and at the last glacial maximum. The distribution of this permafrost-carbon pool is in broad agreement with measurement data for soil carbon content. The level of complexity of the permafrost-carbon model is comparable to other components in the CLIMBER-2 earth system model. |
format |
Article in Journal/Newspaper |
author |
K. A. Crichton D. M. Roche G. Krinner J. Chappellaz |
author_facet |
K. A. Crichton D. M. Roche G. Krinner J. Chappellaz |
author_sort |
K. A. Crichton |
title |
A simplified permafrost-carbon model for long-term climate studies with the CLIMBER-2 coupled earth system model |
title_short |
A simplified permafrost-carbon model for long-term climate studies with the CLIMBER-2 coupled earth system model |
title_full |
A simplified permafrost-carbon model for long-term climate studies with the CLIMBER-2 coupled earth system model |
title_fullStr |
A simplified permafrost-carbon model for long-term climate studies with the CLIMBER-2 coupled earth system model |
title_full_unstemmed |
A simplified permafrost-carbon model for long-term climate studies with the CLIMBER-2 coupled earth system model |
title_sort |
simplified permafrost-carbon model for long-term climate studies with the climber-2 coupled earth system model |
publisher |
Copernicus Publications |
publishDate |
2014 |
url |
https://doi.org/10.5194/gmd-7-3111-2014 https://doaj.org/article/7c13e3287116480ca54d1502a9fe0119 |
genre |
permafrost |
genre_facet |
permafrost |
op_source |
Geoscientific Model Development, Vol 7, Iss 6, Pp 3111-3134 (2014) |
op_relation |
http://www.geosci-model-dev.net/7/3111/2014/gmd-7-3111-2014.pdf https://doaj.org/toc/1991-959X https://doaj.org/toc/1991-9603 1991-959X 1991-9603 doi:10.5194/gmd-7-3111-2014 https://doaj.org/article/7c13e3287116480ca54d1502a9fe0119 |
op_doi |
https://doi.org/10.5194/gmd-7-3111-2014 |
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Geoscientific Model Development |
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7 |
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6 |
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3111 |
op_container_end_page |
3134 |
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