Advancement toward coupling of the VAMPER permafrost model within the Earth system model within the Earth system model iLOVECLIM (version 1.0): description and validation

Abstract. The VU Amsterdam Permafrost (VAMPER) permafrost model has been enhanced with snow thickness and active layer calculations in preparation for coupling within the iLOVECLIM Earth system model of intermediate complexity (EMIC). In addition, maps of basal heat flux and lithology were developed...

Full description

Bibliographic Details
Published in:Geoscientific Model Development
Main Authors: KITOVER, D., VAN BALEN, R., ROCHE, D., VANDENBERGHE, J., RENSSEN, H.
Format: Other/Unknown Material
Language:English
Published: European Geosciences Union 2015
Subjects:
Online Access:https://oskar-bordeaux.fr/handle/20.500.12278/31161
https://doi.org/10.5194/gmd-8-1445-2015
id ftoskarbordeaux:oai:oskar-bordeaux.fr:20.500.12278/31161
record_format openpolar
spelling ftoskarbordeaux:oai:oskar-bordeaux.fr:20.500.12278/31161 2023-05-15T17:55:27+02:00 Advancement toward coupling of the VAMPER permafrost model within the Earth system model within the Earth system model iLOVECLIM (version 1.0): description and validation KITOVER, D. VAN BALEN, R. ROCHE, D. VANDENBERGHE, J. RENSSEN, H. 2015-05-18 https://oskar-bordeaux.fr/handle/20.500.12278/31161 https://doi.org/10.5194/gmd-8-1445-2015 en eng European Geosciences Union 1991-959X https://oskar-bordeaux.fr/handle/20.500.12278/31161 doi:10.5194/gmd-8-1445-2015 Planète et Univers [physics]/Océan Atmosphère Planète et Univers [physics]/Interfaces continentales environnement Article de revue 2015 ftoskarbordeaux https://doi.org/10.5194/gmd-8-1445-2015 2021-05-11T22:29:52Z Abstract. The VU Amsterdam Permafrost (VAMPER) permafrost model has been enhanced with snow thickness and active layer calculations in preparation for coupling within the iLOVECLIM Earth system model of intermediate complexity (EMIC). In addition, maps of basal heat flux and lithology were developed within ECBilt, the atmosphere component of iLOVECLIM, so that VAMPER may use spatially varying parameters of geothermal heat flux and porosity values. The enhanced VAMPER model is validated by comparing the simulated modern-day extent of permafrost thickness with observations. To perform the simulations, the VAMPER model is forced by iLOVECLIM land surface temperatures. Results show that the simulation which did not include the snow cover option overestimated the present permafrost extent. However, when the snow component is included, the simulated permafrost extent is reduced too much. In analyzing simulated permafrost depths, it was found that most of the modeled thickness values and subsurface temperatures fall within a reasonable range of the corresponding observed values. Discrepancies between simulated and observed permafrost depth distribution are due to lack of captured effects from features such as topography and organic soil layers. In addition, some discrepancy is also due to disequilibrium with the current climate, meaning that some observed permafrost is a result of colder states and therefore cannot be reproduced accurately with constant iLOVECLIM preindustrial forcings. Other/Unknown Material permafrost OSKAR Bordeaux (Open Science Knowledge ARchive) Geoscientific Model Development 8 5 1445 1460
institution Open Polar
collection OSKAR Bordeaux (Open Science Knowledge ARchive)
op_collection_id ftoskarbordeaux
language English
topic Planète et Univers [physics]/Océan
Atmosphère
Planète et Univers [physics]/Interfaces continentales
environnement
spellingShingle Planète et Univers [physics]/Océan
Atmosphère
Planète et Univers [physics]/Interfaces continentales
environnement
KITOVER, D.
VAN BALEN, R.
ROCHE, D.
VANDENBERGHE, J.
RENSSEN, H.
Advancement toward coupling of the VAMPER permafrost model within the Earth system model within the Earth system model iLOVECLIM (version 1.0): description and validation
topic_facet Planète et Univers [physics]/Océan
Atmosphère
Planète et Univers [physics]/Interfaces continentales
environnement
description Abstract. The VU Amsterdam Permafrost (VAMPER) permafrost model has been enhanced with snow thickness and active layer calculations in preparation for coupling within the iLOVECLIM Earth system model of intermediate complexity (EMIC). In addition, maps of basal heat flux and lithology were developed within ECBilt, the atmosphere component of iLOVECLIM, so that VAMPER may use spatially varying parameters of geothermal heat flux and porosity values. The enhanced VAMPER model is validated by comparing the simulated modern-day extent of permafrost thickness with observations. To perform the simulations, the VAMPER model is forced by iLOVECLIM land surface temperatures. Results show that the simulation which did not include the snow cover option overestimated the present permafrost extent. However, when the snow component is included, the simulated permafrost extent is reduced too much. In analyzing simulated permafrost depths, it was found that most of the modeled thickness values and subsurface temperatures fall within a reasonable range of the corresponding observed values. Discrepancies between simulated and observed permafrost depth distribution are due to lack of captured effects from features such as topography and organic soil layers. In addition, some discrepancy is also due to disequilibrium with the current climate, meaning that some observed permafrost is a result of colder states and therefore cannot be reproduced accurately with constant iLOVECLIM preindustrial forcings.
format Other/Unknown Material
author KITOVER, D.
VAN BALEN, R.
ROCHE, D.
VANDENBERGHE, J.
RENSSEN, H.
author_facet KITOVER, D.
VAN BALEN, R.
ROCHE, D.
VANDENBERGHE, J.
RENSSEN, H.
author_sort KITOVER, D.
title Advancement toward coupling of the VAMPER permafrost model within the Earth system model within the Earth system model iLOVECLIM (version 1.0): description and validation
title_short Advancement toward coupling of the VAMPER permafrost model within the Earth system model within the Earth system model iLOVECLIM (version 1.0): description and validation
title_full Advancement toward coupling of the VAMPER permafrost model within the Earth system model within the Earth system model iLOVECLIM (version 1.0): description and validation
title_fullStr Advancement toward coupling of the VAMPER permafrost model within the Earth system model within the Earth system model iLOVECLIM (version 1.0): description and validation
title_full_unstemmed Advancement toward coupling of the VAMPER permafrost model within the Earth system model within the Earth system model iLOVECLIM (version 1.0): description and validation
title_sort advancement toward coupling of the vamper permafrost model within the earth system model within the earth system model iloveclim (version 1.0): description and validation
publisher European Geosciences Union
publishDate 2015
url https://oskar-bordeaux.fr/handle/20.500.12278/31161
https://doi.org/10.5194/gmd-8-1445-2015
genre permafrost
genre_facet permafrost
op_relation 1991-959X
https://oskar-bordeaux.fr/handle/20.500.12278/31161
doi:10.5194/gmd-8-1445-2015
op_doi https://doi.org/10.5194/gmd-8-1445-2015
container_title Geoscientific Model Development
container_volume 8
container_issue 5
container_start_page 1445
op_container_end_page 1460
_version_ 1766163401477718016