Freeze/thaw processes in complex permafrost landscapes of northern Siberia simulated using the TEM ecosystem model: impact of thermokarst ponds and lakes

Freeze/thaw (F/T) processes can be quite different under the various land surface types found in the complex tundra of the Arctic, such as polygonal tundra (wet center and dry rims), ponds, and thermokarst lakes. Proper simulation of these different processes is essential for accurate prediction of...

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Published in:Geoscientific Model Development
Main Authors: S. Yi, K. Wischnewski, M. Langer, S. Muster, J. Boike
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2014
Subjects:
Online Access:https://doi.org/10.5194/gmd-7-1671-2014
https://doaj.org/article/5731d05e6ff4492280dbad66ec294a15
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spelling ftdoajarticles:oai:doaj.org/article:5731d05e6ff4492280dbad66ec294a15 2023-05-15T15:09:29+02:00 Freeze/thaw processes in complex permafrost landscapes of northern Siberia simulated using the TEM ecosystem model: impact of thermokarst ponds and lakes S. Yi K. Wischnewski M. Langer S. Muster J. Boike 2014-08-01T00:00:00Z https://doi.org/10.5194/gmd-7-1671-2014 https://doaj.org/article/5731d05e6ff4492280dbad66ec294a15 EN eng Copernicus Publications http://www.geosci-model-dev.net/7/1671/2014/gmd-7-1671-2014.pdf https://doaj.org/toc/1991-959X https://doaj.org/toc/1991-9603 1991-959X 1991-9603 doi:10.5194/gmd-7-1671-2014 https://doaj.org/article/5731d05e6ff4492280dbad66ec294a15 Geoscientific Model Development, Vol 7, Iss 4, Pp 1671-1689 (2014) Geology QE1-996.5 article 2014 ftdoajarticles https://doi.org/10.5194/gmd-7-1671-2014 2022-12-30T23:54:35Z Freeze/thaw (F/T) processes can be quite different under the various land surface types found in the complex tundra of the Arctic, such as polygonal tundra (wet center and dry rims), ponds, and thermokarst lakes. Proper simulation of these different processes is essential for accurate prediction of the release of greenhouse gases under a warming climate scenario. In this study we have incorporated the water layer into a dynamic organic soil version of the Terrestrial Ecosystem Model (DOS-TEM), having first verified and validated the model. Results showed that (1) the DOS-TEM was very efficient and its results compared well with analytical solutions for idealized cases, and (2) despite a number of limitations and uncertainties in the modeling, the simulations compared reasonably well with in situ measurements from polygon rims, polygon centers (with and without water), and lakes on Samoylov Island, Siberia, indicating the suitability of the DOS-TEM for simulating the various F/T processes. Sensitivity tests were performed on the effects of water depth and our results indicated that both water and snow cover are very important in the simulated thermal processes, for both polygon centers and lakes. We therefore concluded that the polygon rims and polygon centers (with various maximum water depths) should be considered separately, and that the dynamics of water depth in both polygons and lakes should be taken into account when simulating thermal processes for methane emission studies. Article in Journal/Newspaper Arctic permafrost Thermokarst Tundra Siberia Directory of Open Access Journals: DOAJ Articles Arctic Geoscientific Model Development 7 4 1671 1689
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Geology
QE1-996.5
spellingShingle Geology
QE1-996.5
S. Yi
K. Wischnewski
M. Langer
S. Muster
J. Boike
Freeze/thaw processes in complex permafrost landscapes of northern Siberia simulated using the TEM ecosystem model: impact of thermokarst ponds and lakes
topic_facet Geology
QE1-996.5
description Freeze/thaw (F/T) processes can be quite different under the various land surface types found in the complex tundra of the Arctic, such as polygonal tundra (wet center and dry rims), ponds, and thermokarst lakes. Proper simulation of these different processes is essential for accurate prediction of the release of greenhouse gases under a warming climate scenario. In this study we have incorporated the water layer into a dynamic organic soil version of the Terrestrial Ecosystem Model (DOS-TEM), having first verified and validated the model. Results showed that (1) the DOS-TEM was very efficient and its results compared well with analytical solutions for idealized cases, and (2) despite a number of limitations and uncertainties in the modeling, the simulations compared reasonably well with in situ measurements from polygon rims, polygon centers (with and without water), and lakes on Samoylov Island, Siberia, indicating the suitability of the DOS-TEM for simulating the various F/T processes. Sensitivity tests were performed on the effects of water depth and our results indicated that both water and snow cover are very important in the simulated thermal processes, for both polygon centers and lakes. We therefore concluded that the polygon rims and polygon centers (with various maximum water depths) should be considered separately, and that the dynamics of water depth in both polygons and lakes should be taken into account when simulating thermal processes for methane emission studies.
format Article in Journal/Newspaper
author S. Yi
K. Wischnewski
M. Langer
S. Muster
J. Boike
author_facet S. Yi
K. Wischnewski
M. Langer
S. Muster
J. Boike
author_sort S. Yi
title Freeze/thaw processes in complex permafrost landscapes of northern Siberia simulated using the TEM ecosystem model: impact of thermokarst ponds and lakes
title_short Freeze/thaw processes in complex permafrost landscapes of northern Siberia simulated using the TEM ecosystem model: impact of thermokarst ponds and lakes
title_full Freeze/thaw processes in complex permafrost landscapes of northern Siberia simulated using the TEM ecosystem model: impact of thermokarst ponds and lakes
title_fullStr Freeze/thaw processes in complex permafrost landscapes of northern Siberia simulated using the TEM ecosystem model: impact of thermokarst ponds and lakes
title_full_unstemmed Freeze/thaw processes in complex permafrost landscapes of northern Siberia simulated using the TEM ecosystem model: impact of thermokarst ponds and lakes
title_sort freeze/thaw processes in complex permafrost landscapes of northern siberia simulated using the tem ecosystem model: impact of thermokarst ponds and lakes
publisher Copernicus Publications
publishDate 2014
url https://doi.org/10.5194/gmd-7-1671-2014
https://doaj.org/article/5731d05e6ff4492280dbad66ec294a15
geographic Arctic
geographic_facet Arctic
genre Arctic
permafrost
Thermokarst
Tundra
Siberia
genre_facet Arctic
permafrost
Thermokarst
Tundra
Siberia
op_source Geoscientific Model Development, Vol 7, Iss 4, Pp 1671-1689 (2014)
op_relation http://www.geosci-model-dev.net/7/1671/2014/gmd-7-1671-2014.pdf
https://doaj.org/toc/1991-959X
https://doaj.org/toc/1991-9603
1991-959X
1991-9603
doi:10.5194/gmd-7-1671-2014
https://doaj.org/article/5731d05e6ff4492280dbad66ec294a15
op_doi https://doi.org/10.5194/gmd-7-1671-2014
container_title Geoscientific Model Development
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