Impact of measured and simulated tundra snowpack properties on heat transfer

Snowpack microstructure controls the transfer of heat to, as well as the temperature of, the underlying soils. In situ measurements of snow and soil properties from four field campaigns during two winters (March and November 2018, January and March 2019) were compared to an ensemble of CLM5.0 (Commu...

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Published in:The Cryosphere
Main Authors: Dutch, Victoria R., Rutter, Nick, Wake, Leanne, Sandells, Melody, Derksen, Chris, Walker, Branden, Hould Gosselin, Gabriel, Sonnentag, Oliver, Essery, Richard, Kelly, Richard, Marsh, Phillip, King, Joshua, Boike, Julia
Format: Text
Language:English
Published: 2022
Subjects:
Online Access:https://doi.org/10.5194/tc-16-4201-2022
https://tc.copernicus.org/articles/16/4201/2022/
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spelling ftcopernicus:oai:publications.copernicus.org:tc98070 2023-05-15T17:46:45+02:00 Impact of measured and simulated tundra snowpack properties on heat transfer Dutch, Victoria R. Rutter, Nick Wake, Leanne Sandells, Melody Derksen, Chris Walker, Branden Hould Gosselin, Gabriel Sonnentag, Oliver Essery, Richard Kelly, Richard Marsh, Phillip King, Joshua Boike, Julia 2022-10-11 application/pdf https://doi.org/10.5194/tc-16-4201-2022 https://tc.copernicus.org/articles/16/4201/2022/ eng eng doi:10.5194/tc-16-4201-2022 https://tc.copernicus.org/articles/16/4201/2022/ eISSN: 1994-0424 Text 2022 ftcopernicus https://doi.org/10.5194/tc-16-4201-2022 2022-10-17T16:22:44Z Snowpack microstructure controls the transfer of heat to, as well as the temperature of, the underlying soils. In situ measurements of snow and soil properties from four field campaigns during two winters (March and November 2018, January and March 2019) were compared to an ensemble of CLM5.0 (Community Land Model) simulations, at Trail Valley Creek, Northwest Territories, Canada. Snow micropenetrometer profiles allowed for snowpack density and thermal conductivity to be derived at higher vertical resolution (1.25 mm) and a larger sample size ( n =1050 ) compared to traditional snowpit observations (3 cm vertical resolution; n =115 ). Comparing measurements with simulations shows CLM overestimated snow thermal conductivity by a factor of 3, leading to a cold bias in wintertime soil temperatures ( RMSE=5.8 ∘ C). Two different approaches were taken to reduce this bias: alternative parameterisations of snow thermal conductivity and the application of a correction factor. All the evaluated parameterisations of snow thermal conductivity improved simulations of wintertime soil temperatures, with that of Sturm et al. (1997) having the greatest impact ( RMSE=2.5 ∘ C). The required correction factor is strongly related to snow depth ( <math xmlns="http://www.w3.org/1998/Math/MathML" id="M7" display="inline" overflow="scroll" dspmath="mathml"><mrow><msup><mi>R</mi><mn mathvariant="normal">2</mn></msup><mo>=</mo><mn mathvariant="normal">0.77</mn><mo>,</mo><mi mathvariant="normal">RMSE</mi><mo>=</mo><mn mathvariant="normal">0.066</mn></mrow></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="125pt" height="15pt" class="svg-formula" dspmath="mathimg" md5hash="43542648a66c7c68c7e864927fbc13df"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="tc-16-4201-2022-ie00001.svg" width="125pt" height="15pt" src="tc-16-4201-2022-ie00001.png"/></svg:svg> ) and ... Text Northwest Territories Tundra Copernicus Publications: E-Journals Canada Northwest Territories Sturm ENVELOPE(162.967,162.967,-71.050,-71.050) Trail Valley Creek ENVELOPE(-133.415,-133.415,68.772,68.772) Valley Creek ENVELOPE(-138.324,-138.324,63.326,63.326) The Cryosphere 16 10 4201 4222
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description Snowpack microstructure controls the transfer of heat to, as well as the temperature of, the underlying soils. In situ measurements of snow and soil properties from four field campaigns during two winters (March and November 2018, January and March 2019) were compared to an ensemble of CLM5.0 (Community Land Model) simulations, at Trail Valley Creek, Northwest Territories, Canada. Snow micropenetrometer profiles allowed for snowpack density and thermal conductivity to be derived at higher vertical resolution (1.25 mm) and a larger sample size ( n =1050 ) compared to traditional snowpit observations (3 cm vertical resolution; n =115 ). Comparing measurements with simulations shows CLM overestimated snow thermal conductivity by a factor of 3, leading to a cold bias in wintertime soil temperatures ( RMSE=5.8 ∘ C). Two different approaches were taken to reduce this bias: alternative parameterisations of snow thermal conductivity and the application of a correction factor. All the evaluated parameterisations of snow thermal conductivity improved simulations of wintertime soil temperatures, with that of Sturm et al. (1997) having the greatest impact ( RMSE=2.5 ∘ C). The required correction factor is strongly related to snow depth ( <math xmlns="http://www.w3.org/1998/Math/MathML" id="M7" display="inline" overflow="scroll" dspmath="mathml"><mrow><msup><mi>R</mi><mn mathvariant="normal">2</mn></msup><mo>=</mo><mn mathvariant="normal">0.77</mn><mo>,</mo><mi mathvariant="normal">RMSE</mi><mo>=</mo><mn mathvariant="normal">0.066</mn></mrow></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="125pt" height="15pt" class="svg-formula" dspmath="mathimg" md5hash="43542648a66c7c68c7e864927fbc13df"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="tc-16-4201-2022-ie00001.svg" width="125pt" height="15pt" src="tc-16-4201-2022-ie00001.png"/></svg:svg> ) and ...
format Text
author Dutch, Victoria R.
Rutter, Nick
Wake, Leanne
Sandells, Melody
Derksen, Chris
Walker, Branden
Hould Gosselin, Gabriel
Sonnentag, Oliver
Essery, Richard
Kelly, Richard
Marsh, Phillip
King, Joshua
Boike, Julia
spellingShingle Dutch, Victoria R.
Rutter, Nick
Wake, Leanne
Sandells, Melody
Derksen, Chris
Walker, Branden
Hould Gosselin, Gabriel
Sonnentag, Oliver
Essery, Richard
Kelly, Richard
Marsh, Phillip
King, Joshua
Boike, Julia
Impact of measured and simulated tundra snowpack properties on heat transfer
author_facet Dutch, Victoria R.
Rutter, Nick
Wake, Leanne
Sandells, Melody
Derksen, Chris
Walker, Branden
Hould Gosselin, Gabriel
Sonnentag, Oliver
Essery, Richard
Kelly, Richard
Marsh, Phillip
King, Joshua
Boike, Julia
author_sort Dutch, Victoria R.
title Impact of measured and simulated tundra snowpack properties on heat transfer
title_short Impact of measured and simulated tundra snowpack properties on heat transfer
title_full Impact of measured and simulated tundra snowpack properties on heat transfer
title_fullStr Impact of measured and simulated tundra snowpack properties on heat transfer
title_full_unstemmed Impact of measured and simulated tundra snowpack properties on heat transfer
title_sort impact of measured and simulated tundra snowpack properties on heat transfer
publishDate 2022
url https://doi.org/10.5194/tc-16-4201-2022
https://tc.copernicus.org/articles/16/4201/2022/
long_lat ENVELOPE(162.967,162.967,-71.050,-71.050)
ENVELOPE(-133.415,-133.415,68.772,68.772)
ENVELOPE(-138.324,-138.324,63.326,63.326)
geographic Canada
Northwest Territories
Sturm
Trail Valley Creek
Valley Creek
geographic_facet Canada
Northwest Territories
Sturm
Trail Valley Creek
Valley Creek
genre Northwest Territories
Tundra
genre_facet Northwest Territories
Tundra
op_source eISSN: 1994-0424
op_relation doi:10.5194/tc-16-4201-2022
https://tc.copernicus.org/articles/16/4201/2022/
op_doi https://doi.org/10.5194/tc-16-4201-2022
container_title The Cryosphere
container_volume 16
container_issue 10
container_start_page 4201
op_container_end_page 4222
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