Drying of tundra landscapes will limit subsidence-induced acceleration of permafrost thaw: Modeling Archive

This Modeling Archive is in support of a NGEE Arctic publication in review “ Drying of tundra landscapes will limit subsidence-induced acceleration of permafrost thaw ”. The study used a cryohydrology model to assess the potential risk of abrupt permafrost thaw triggered by melting ground ice, a key...

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Main Authors: Painter, Scott, Jan, Ahmad, Coon, Ethan
Language:unknown
Published: 2023
Subjects:
Ice
Online Access:http://www.osti.gov/servlets/purl/1876200
https://www.osti.gov/biblio/1876200
https://doi.org/10.5440/1876200
id ftosti:oai:osti.gov:1876200
record_format openpolar
spelling ftosti:oai:osti.gov:1876200 2023-07-30T04:00:32+02:00 Drying of tundra landscapes will limit subsidence-induced acceleration of permafrost thaw: Modeling Archive Painter, Scott Jan, Ahmad Coon, Ethan 2023-03-02 application/pdf http://www.osti.gov/servlets/purl/1876200 https://www.osti.gov/biblio/1876200 https://doi.org/10.5440/1876200 unknown http://www.osti.gov/servlets/purl/1876200 https://www.osti.gov/biblio/1876200 https://doi.org/10.5440/1876200 doi:10.5440/1876200 54 Environmental Sciences 2023 ftosti https://doi.org/10.5440/1876200 2023-07-11T10:13:27Z This Modeling Archive is in support of a NGEE Arctic publication in review “ Drying of tundra landscapes will limit subsidence-induced acceleration of permafrost thaw ”. The study used a cryohydrology model to assess the potential risk of abrupt permafrost thaw triggered by melting ground ice, a key open question associated with permafrost response to a warming Arctic. The spatially resolved simulations are for a small catchment 465 ice-wedge polygons in polygonal tundra near Utqiaġvik, Alaska in the high-emissions RCP8.5 climate scenario. The simulations are compared to runoff, evapotranspiration and subsidence in the current climate and agree well. The study used the ATS code configured as an intermediate-scale cryohydrology model (Advanced Terrestrial Simulator, Version ngee_ism_v2 https://github.com/amanzi/amanzi/releases/tag/ngee_ism_v2 ). The archive includes input files for spinup (1985 to 2005) and projections (2006 to 2100 – the manuscript reports 2006 to 2098). Three of the projections include the effects of subsidence and microtopography change with different depth profiles of ice content corresponding to the median, 20th percentile and 80th percentile. The fourth projection has subsidence turnoff and uses the reference case (median) ice content. Spatially averaged or aggregated output variables are included for the projections. Selected checkpoint files for the projections and postprocessing scripts are also included. Files included are *.xml; *.h5; *.exo; *.py; *.sh, *. nb, mesh files, and a tar.gz file. The Next-Generation Ecosystem Experiments: Arctic (NGEE Arctic), was a research effort to reduce uncertainty in Earth System Models by developing a predictive understanding of carbon-rich Arctic ecosystems and feedbacks to climate. NGEE Arctic was supported by the Department of Energy's Office of Biological and Environmental Research. The NGEE Arctic project had two field research sites: 1) located within the Arctic polygonal tundra coastal region on the Barrow Environmental Observatory (BEO) and ... Other/Unknown Material Arctic Barrow Ice permafrost Tundra wedge* Alaska SciTec Connect (Office of Scientific and Technical Information - OSTI, U.S. Department of Energy) Arctic
institution Open Polar
collection SciTec Connect (Office of Scientific and Technical Information - OSTI, U.S. Department of Energy)
op_collection_id ftosti
language unknown
topic 54 Environmental Sciences
spellingShingle 54 Environmental Sciences
Painter, Scott
Jan, Ahmad
Coon, Ethan
Drying of tundra landscapes will limit subsidence-induced acceleration of permafrost thaw: Modeling Archive
topic_facet 54 Environmental Sciences
description This Modeling Archive is in support of a NGEE Arctic publication in review “ Drying of tundra landscapes will limit subsidence-induced acceleration of permafrost thaw ”. The study used a cryohydrology model to assess the potential risk of abrupt permafrost thaw triggered by melting ground ice, a key open question associated with permafrost response to a warming Arctic. The spatially resolved simulations are for a small catchment 465 ice-wedge polygons in polygonal tundra near Utqiaġvik, Alaska in the high-emissions RCP8.5 climate scenario. The simulations are compared to runoff, evapotranspiration and subsidence in the current climate and agree well. The study used the ATS code configured as an intermediate-scale cryohydrology model (Advanced Terrestrial Simulator, Version ngee_ism_v2 https://github.com/amanzi/amanzi/releases/tag/ngee_ism_v2 ). The archive includes input files for spinup (1985 to 2005) and projections (2006 to 2100 – the manuscript reports 2006 to 2098). Three of the projections include the effects of subsidence and microtopography change with different depth profiles of ice content corresponding to the median, 20th percentile and 80th percentile. The fourth projection has subsidence turnoff and uses the reference case (median) ice content. Spatially averaged or aggregated output variables are included for the projections. Selected checkpoint files for the projections and postprocessing scripts are also included. Files included are *.xml; *.h5; *.exo; *.py; *.sh, *. nb, mesh files, and a tar.gz file. The Next-Generation Ecosystem Experiments: Arctic (NGEE Arctic), was a research effort to reduce uncertainty in Earth System Models by developing a predictive understanding of carbon-rich Arctic ecosystems and feedbacks to climate. NGEE Arctic was supported by the Department of Energy's Office of Biological and Environmental Research. The NGEE Arctic project had two field research sites: 1) located within the Arctic polygonal tundra coastal region on the Barrow Environmental Observatory (BEO) and ...
author Painter, Scott
Jan, Ahmad
Coon, Ethan
author_facet Painter, Scott
Jan, Ahmad
Coon, Ethan
author_sort Painter, Scott
title Drying of tundra landscapes will limit subsidence-induced acceleration of permafrost thaw: Modeling Archive
title_short Drying of tundra landscapes will limit subsidence-induced acceleration of permafrost thaw: Modeling Archive
title_full Drying of tundra landscapes will limit subsidence-induced acceleration of permafrost thaw: Modeling Archive
title_fullStr Drying of tundra landscapes will limit subsidence-induced acceleration of permafrost thaw: Modeling Archive
title_full_unstemmed Drying of tundra landscapes will limit subsidence-induced acceleration of permafrost thaw: Modeling Archive
title_sort drying of tundra landscapes will limit subsidence-induced acceleration of permafrost thaw: modeling archive
publishDate 2023
url http://www.osti.gov/servlets/purl/1876200
https://www.osti.gov/biblio/1876200
https://doi.org/10.5440/1876200
geographic Arctic
geographic_facet Arctic
genre Arctic
Barrow
Ice
permafrost
Tundra
wedge*
Alaska
genre_facet Arctic
Barrow
Ice
permafrost
Tundra
wedge*
Alaska
op_relation http://www.osti.gov/servlets/purl/1876200
https://www.osti.gov/biblio/1876200
https://doi.org/10.5440/1876200
doi:10.5440/1876200
op_doi https://doi.org/10.5440/1876200
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