Towards representing thermokarst processes in land surface models

Large-scale Earth system and land surface models often lack an adequate representation of subgrid-scale processes in permafrost landscapes. Small-scale processes such as thermokarst formation might, however, considerably impact the energy and carbon budgets in way which is not resolved within large-...

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Main Authors: Nitzbon, Jan, Langer, Moritz, Westermann, Sebastian, Grosse, Guido, Boike, Julia
Format: Conference Object
Language:unknown
Published: 2017
Subjects:
Ice
Online Access:https://epic.awi.de/id/eprint/44632/
https://epic.awi.de/id/eprint/44632/1/Nitzbon_csdms_poster_A0_final.pdf
https://hdl.handle.net/10013/epic.50914
https://hdl.handle.net/10013/epic.50914.d001
id ftawi:oai:epic.awi.de:44632
record_format openpolar
spelling ftawi:oai:epic.awi.de:44632 2023-05-15T16:37:18+02:00 Towards representing thermokarst processes in land surface models Nitzbon, Jan Langer, Moritz Westermann, Sebastian Grosse, Guido Boike, Julia 2017-05-24 application/pdf https://epic.awi.de/id/eprint/44632/ https://epic.awi.de/id/eprint/44632/1/Nitzbon_csdms_poster_A0_final.pdf https://hdl.handle.net/10013/epic.50914 https://hdl.handle.net/10013/epic.50914.d001 unknown https://epic.awi.de/id/eprint/44632/1/Nitzbon_csdms_poster_A0_final.pdf https://hdl.handle.net/10013/epic.50914.d001 Nitzbon, J. orcid:0000-0001-7205-6298 , Langer, M. orcid:0000-0002-2704-3655 , Westermann, S. , Grosse, G. orcid:0000-0001-5895-2141 and Boike, J. orcid:0000-0002-5875-2112 (2017) Towards representing thermokarst processes in land surface models , Community Surface Dynamics Modeling System Annual Meeting, Boulder, Colorado, USA, 23 May 2017 - 25 May 2017 . hdl:10013/epic.50914 EPIC3Community Surface Dynamics Modeling System Annual Meeting, Boulder, Colorado, USA, 2017-05-23-2017-05-25 Conference notRev 2017 ftawi 2021-12-24T15:42:58Z Large-scale Earth system and land surface models often lack an adequate representation of subgrid-scale processes in permafrost landscapes. Small-scale processes such as thermokarst formation might, however, considerably impact the energy and carbon budgets in way which is not resolved within large-scale models. Since a spatially high-resolved simulation of such processes is not feasible, novel techniques for up-scaling subgrid processes are demanded. Within this work a one-dimensional model of the ground thermal regime of land surfaces, CryoGrid 3, is employed to conceptually represent small-scale features of permafrost landscapes, particularly those related to thermokarst. For example, the model has been shown to adequately describe the degradation of permafrost underneath waterbodies in a warming climate. Using tiling approaches such point-wise realizations can be up-scaled in a statistical way in order to represent larger land surface units. The model development is closely linked to field campaigns to the Lena River Delta in Siberia which offers very diverse land surface features such as polygonal tundra and thermos-erosional valleys. These features are related to the region’s diverse soil stratigraphies, in particular the occurrence of ice-rich ground. Combining field measurements with modelling ultimately allows an improvement in the qualitative and quantitative understanding of the typical geomorphological processes in permafrost landscapes and their representation in large-scale models. Conference Object Ice lena river permafrost Thermokarst Tundra Siberia Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center)
institution Open Polar
collection Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center)
op_collection_id ftawi
language unknown
description Large-scale Earth system and land surface models often lack an adequate representation of subgrid-scale processes in permafrost landscapes. Small-scale processes such as thermokarst formation might, however, considerably impact the energy and carbon budgets in way which is not resolved within large-scale models. Since a spatially high-resolved simulation of such processes is not feasible, novel techniques for up-scaling subgrid processes are demanded. Within this work a one-dimensional model of the ground thermal regime of land surfaces, CryoGrid 3, is employed to conceptually represent small-scale features of permafrost landscapes, particularly those related to thermokarst. For example, the model has been shown to adequately describe the degradation of permafrost underneath waterbodies in a warming climate. Using tiling approaches such point-wise realizations can be up-scaled in a statistical way in order to represent larger land surface units. The model development is closely linked to field campaigns to the Lena River Delta in Siberia which offers very diverse land surface features such as polygonal tundra and thermos-erosional valleys. These features are related to the region’s diverse soil stratigraphies, in particular the occurrence of ice-rich ground. Combining field measurements with modelling ultimately allows an improvement in the qualitative and quantitative understanding of the typical geomorphological processes in permafrost landscapes and their representation in large-scale models.
format Conference Object
author Nitzbon, Jan
Langer, Moritz
Westermann, Sebastian
Grosse, Guido
Boike, Julia
spellingShingle Nitzbon, Jan
Langer, Moritz
Westermann, Sebastian
Grosse, Guido
Boike, Julia
Towards representing thermokarst processes in land surface models
author_facet Nitzbon, Jan
Langer, Moritz
Westermann, Sebastian
Grosse, Guido
Boike, Julia
author_sort Nitzbon, Jan
title Towards representing thermokarst processes in land surface models
title_short Towards representing thermokarst processes in land surface models
title_full Towards representing thermokarst processes in land surface models
title_fullStr Towards representing thermokarst processes in land surface models
title_full_unstemmed Towards representing thermokarst processes in land surface models
title_sort towards representing thermokarst processes in land surface models
publishDate 2017
url https://epic.awi.de/id/eprint/44632/
https://epic.awi.de/id/eprint/44632/1/Nitzbon_csdms_poster_A0_final.pdf
https://hdl.handle.net/10013/epic.50914
https://hdl.handle.net/10013/epic.50914.d001
genre Ice
lena river
permafrost
Thermokarst
Tundra
Siberia
genre_facet Ice
lena river
permafrost
Thermokarst
Tundra
Siberia
op_source EPIC3Community Surface Dynamics Modeling System Annual Meeting, Boulder, Colorado, USA, 2017-05-23-2017-05-25
op_relation https://epic.awi.de/id/eprint/44632/1/Nitzbon_csdms_poster_A0_final.pdf
https://hdl.handle.net/10013/epic.50914.d001
Nitzbon, J. orcid:0000-0001-7205-6298 , Langer, M. orcid:0000-0002-2704-3655 , Westermann, S. , Grosse, G. orcid:0000-0001-5895-2141 and Boike, J. orcid:0000-0002-5875-2112 (2017) Towards representing thermokarst processes in land surface models , Community Surface Dynamics Modeling System Annual Meeting, Boulder, Colorado, USA, 23 May 2017 - 25 May 2017 . hdl:10013/epic.50914
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