Coupled multilayer canopy-permafrost model (CryoGrid) for the use in permafrost underlain boreal forests.

CryoGrid is a land-surface scheme dedicated to modeling of ground temperatures in permafrost environments. Here, the one-dimensional land surface model (CryoGrid) is adapted for the application in vegetated areas by coupling a multilayer canopy model (CLM-ml v0). This model setup is used to reproduc...

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Main Authors: Stuenzi, Simone M., Boike, Julia, Cable, William, Herzschuh, Ulrike, Kruse, Stefan, Pestryakova, Luidmila A., Schneider von Deimling, Thomas, Westermann, Sebastian, Zakharov, Evgeniy S., Langer, Moritz
Format: Article in Journal/Newspaper
Language:English
Published: Zenodo 2020
Subjects:
Ice
Online Access:https://dx.doi.org/10.5281/zenodo.4317107
https://zenodo.org/record/4317107
id ftdatacite:10.5281/zenodo.4317107
record_format openpolar
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Permafrost
Land surface model
CryoGrid
Boreal forest
spellingShingle Permafrost
Land surface model
CryoGrid
Boreal forest
Stuenzi, Simone M.
Boike, Julia
Cable, William
Herzschuh, Ulrike
Kruse, Stefan
Pestryakova, Luidmila A.
Schneider von Deimling, Thomas
Westermann, Sebastian
Zakharov, Evgeniy S.
Langer, Moritz
Coupled multilayer canopy-permafrost model (CryoGrid) for the use in permafrost underlain boreal forests.
topic_facet Permafrost
Land surface model
CryoGrid
Boreal forest
description CryoGrid is a land-surface scheme dedicated to modeling of ground temperatures in permafrost environments. Here, the one-dimensional land surface model (CryoGrid) is adapted for the application in vegetated areas by coupling a multilayer canopy model (CLM-ml v0). This model setup is used to reproduce the energy transfer and thermal regime at a study site in mixed boreal forest in Eastern Siberia. The vegetation module forms the upper boundary layer of the coupled vegetation-permafrost model and replaces the surface energy balance equation used for common CryoGrid representations. The model is described in the following article which has been published in Biogeosciences: Stuenzi, S. M., Boike, J., Cable, W., Herzschuh, U., Kruse, S., Pestryakova, L. A., Schneider von Deimling, T., Westermann, S., Zakharov, E. S., and Langer, M.: Variability of the surface energy balance in permafrost-underlain boreal forest, Biogeosciences, 18, 343–365, https://doi.org/10.5194/bg-18-343-2021, 2021. The parameters are set to the default values that were used for the simulations in the article. Parameters different from the default values can be specified in the main script main.m (general parameters, run number, etc.) and in the excel table \results\test_oldCG_334\ test_oldCG_334.xlsx (run-specific parameters). To start the program, run the script main.m . The default output directory is .\results\. Further updates to the model code can be found here: https://github.com/CryoGrid/CryoGrid/tree/vegetation Updates and documentation of the Permafrost model CryoGrid can be found here: https://github.com/CryoGrid. The model is further described in this publication: Westermann, S., Langer, M., Boike, J., Heikenfeld, M., Peter, M., Etzelmüller, B., & Krinner, G. (2016). Simulating the thermal regime and thaw processes of ice-rich permafrost ground with the land-surface model CryoGrid 3. Geosci. Model Dev. , 9(2), 523–546. https://doi.org/10.5194/gmd-9-523-2016. The multilayer canopy model was first published by Bonan et al. (2018) : Modeling canopy-induced turbulence in the Earth system: a unified parameterization of turbulent exchange within plant canopies and the roughness sublayer (CLM-ml v0) (https://doi.org/10.5194/gmd-11-1467-2018). : {"references": ["Stuenzi et al. (2021):\u00a0Variability of the Surface Energy Balance in Permafrost Underlain Boreal Forest\u00a0(DOI:\u00a010.5194/bg-2020-201)", "Bonan et al. (2018):\u00a0Modeling canopy-induced turbulence in the Earth system: a unified parameterization of turbulent exchange within plant canopies and the roughness sublayer (CLM-ml v0) (DOI: 10.5194/gmd-11-1467-2018)", "Westermann et al. (2013):\u00a0Transient thermal modeling of permafrost conditions in Southern Norway (DOI: 10.5194/tc-7-719-2013)"]}
format Article in Journal/Newspaper
author Stuenzi, Simone M.
Boike, Julia
Cable, William
Herzschuh, Ulrike
Kruse, Stefan
Pestryakova, Luidmila A.
Schneider von Deimling, Thomas
Westermann, Sebastian
Zakharov, Evgeniy S.
Langer, Moritz
author_facet Stuenzi, Simone M.
Boike, Julia
Cable, William
Herzschuh, Ulrike
Kruse, Stefan
Pestryakova, Luidmila A.
Schneider von Deimling, Thomas
Westermann, Sebastian
Zakharov, Evgeniy S.
Langer, Moritz
author_sort Stuenzi, Simone M.
title Coupled multilayer canopy-permafrost model (CryoGrid) for the use in permafrost underlain boreal forests.
title_short Coupled multilayer canopy-permafrost model (CryoGrid) for the use in permafrost underlain boreal forests.
title_full Coupled multilayer canopy-permafrost model (CryoGrid) for the use in permafrost underlain boreal forests.
title_fullStr Coupled multilayer canopy-permafrost model (CryoGrid) for the use in permafrost underlain boreal forests.
title_full_unstemmed Coupled multilayer canopy-permafrost model (CryoGrid) for the use in permafrost underlain boreal forests.
title_sort coupled multilayer canopy-permafrost model (cryogrid) for the use in permafrost underlain boreal forests.
publisher Zenodo
publishDate 2020
url https://dx.doi.org/10.5281/zenodo.4317107
https://zenodo.org/record/4317107
long_lat ENVELOPE(130.617,130.617,64.650,64.650)
geographic Norway
Zakharov
geographic_facet Norway
Zakharov
genre Ice
permafrost
Siberia
genre_facet Ice
permafrost
Siberia
op_relation https://github.com/CryoGrid/CryoGrid/tree/vegetation
https://github.com/CryoGrid/CryoGrid/tree/vegetation
https://dx.doi.org/10.5194/bg-2020-201
https://dx.doi.org/10.1594/pangaea.919859
https://dx.doi.org/10.1594/pangaea.914327
https://dx.doi.org/10.5281/zenodo.4317106
op_rights Open Access
Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
info:eu-repo/semantics/openAccess
op_rightsnorm CC-BY
op_doi https://doi.org/10.5281/zenodo.4317107
https://doi.org/10.5194/bg-2020-201
https://doi.org/10.1594/pangaea.919859
https://doi.org/10.1594/pangaea.914327
https://doi.org/10.5281/zenodo.4317106
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spelling ftdatacite:10.5281/zenodo.4317107 2023-05-15T16:37:21+02:00 Coupled multilayer canopy-permafrost model (CryoGrid) for the use in permafrost underlain boreal forests. Stuenzi, Simone M. Boike, Julia Cable, William Herzschuh, Ulrike Kruse, Stefan Pestryakova, Luidmila A. Schneider von Deimling, Thomas Westermann, Sebastian Zakharov, Evgeniy S. Langer, Moritz 2020 https://dx.doi.org/10.5281/zenodo.4317107 https://zenodo.org/record/4317107 en eng Zenodo https://github.com/CryoGrid/CryoGrid/tree/vegetation https://github.com/CryoGrid/CryoGrid/tree/vegetation https://dx.doi.org/10.5194/bg-2020-201 https://dx.doi.org/10.1594/pangaea.919859 https://dx.doi.org/10.1594/pangaea.914327 https://dx.doi.org/10.5281/zenodo.4317106 Open Access Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 info:eu-repo/semantics/openAccess CC-BY Permafrost Land surface model CryoGrid Boreal forest Software SoftwareSourceCode article 2020 ftdatacite https://doi.org/10.5281/zenodo.4317107 https://doi.org/10.5194/bg-2020-201 https://doi.org/10.1594/pangaea.919859 https://doi.org/10.1594/pangaea.914327 https://doi.org/10.5281/zenodo.4317106 2021-11-05T12:55:41Z CryoGrid is a land-surface scheme dedicated to modeling of ground temperatures in permafrost environments. Here, the one-dimensional land surface model (CryoGrid) is adapted for the application in vegetated areas by coupling a multilayer canopy model (CLM-ml v0). This model setup is used to reproduce the energy transfer and thermal regime at a study site in mixed boreal forest in Eastern Siberia. The vegetation module forms the upper boundary layer of the coupled vegetation-permafrost model and replaces the surface energy balance equation used for common CryoGrid representations. The model is described in the following article which has been published in Biogeosciences: Stuenzi, S. M., Boike, J., Cable, W., Herzschuh, U., Kruse, S., Pestryakova, L. A., Schneider von Deimling, T., Westermann, S., Zakharov, E. S., and Langer, M.: Variability of the surface energy balance in permafrost-underlain boreal forest, Biogeosciences, 18, 343–365, https://doi.org/10.5194/bg-18-343-2021, 2021. The parameters are set to the default values that were used for the simulations in the article. Parameters different from the default values can be specified in the main script main.m (general parameters, run number, etc.) and in the excel table \results\test_oldCG_334\ test_oldCG_334.xlsx (run-specific parameters). To start the program, run the script main.m . The default output directory is .\results\. Further updates to the model code can be found here: https://github.com/CryoGrid/CryoGrid/tree/vegetation Updates and documentation of the Permafrost model CryoGrid can be found here: https://github.com/CryoGrid. The model is further described in this publication: Westermann, S., Langer, M., Boike, J., Heikenfeld, M., Peter, M., Etzelmüller, B., & Krinner, G. (2016). Simulating the thermal regime and thaw processes of ice-rich permafrost ground with the land-surface model CryoGrid 3. Geosci. Model Dev. , 9(2), 523–546. https://doi.org/10.5194/gmd-9-523-2016. The multilayer canopy model was first published by Bonan et al. (2018) : Modeling canopy-induced turbulence in the Earth system: a unified parameterization of turbulent exchange within plant canopies and the roughness sublayer (CLM-ml v0) (https://doi.org/10.5194/gmd-11-1467-2018). : {"references": ["Stuenzi et al. (2021):\u00a0Variability of the Surface Energy Balance in Permafrost Underlain Boreal Forest\u00a0(DOI:\u00a010.5194/bg-2020-201)", "Bonan et al. (2018):\u00a0Modeling canopy-induced turbulence in the Earth system: a unified parameterization of turbulent exchange within plant canopies and the roughness sublayer (CLM-ml v0) (DOI: 10.5194/gmd-11-1467-2018)", "Westermann et al. (2013):\u00a0Transient thermal modeling of permafrost conditions in Southern Norway (DOI: 10.5194/tc-7-719-2013)"]} Article in Journal/Newspaper Ice permafrost Siberia DataCite Metadata Store (German National Library of Science and Technology) Norway Zakharov ENVELOPE(130.617,130.617,64.650,64.650)