Modeling the winter heat conduction through the sea ice system during MOSAiC

Models struggle to accurately simulate observed sea ice thickness changes, which could be partially due to inadequate representation of thermodynamic processes. We analyzed co-located winter observations of the Arctic sea ice from the Multidisciplinary Drifting Observatory for the Study of the Arcti...

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Published in:Geophysical Research Letters
Other Authors: Zampieri, Lorenzo (author), Clemens‐Sewall, David (author), Sledd, Anne (author), Hutter, Nils (author), Holland, Marika (author)
Format: Article in Journal/Newspaper
Language:English
Published: 2024
Subjects:
Online Access:https://doi.org/10.1029/2023GL106760
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spelling ftncar:oai:drupal-site.org:articles_27163 2024-06-23T07:49:56+00:00 Modeling the winter heat conduction through the sea ice system during MOSAiC Zampieri, Lorenzo (author) Clemens‐Sewall, David (author) Sledd, Anne (author) Hutter, Nils (author) Holland, Marika (author) 2024-04-28 https://doi.org/10.1029/2023GL106760 en eng Geophysical Research Letters--Geophysical Research Letters--0094-8276--1944-8007 articles:27163 doi:10.1029/2023GL106760 ark:/85065/d7sx6jdv Copyright author(s). This work is licensed under a Creative Commons Attribution-NonCommercial 4.0 International License. article Text 2024 ftncar https://doi.org/10.1029/2023GL106760 2024-05-27T14:15:41Z Models struggle to accurately simulate observed sea ice thickness changes, which could be partially due to inadequate representation of thermodynamic processes. We analyzed co-located winter observations of the Arctic sea ice from the Multidisciplinary Drifting Observatory for the Study of the Arctic Climate for evaluating and improving thermodynamic processes in sea ice models, aiming to enable more accurate predictions of the warming climate system. We model the sea ice and snow heat conduction for observed transects forced by realistic boundary conditions to understand the impact of the non-resolved meter-scale snow and sea ice thickness heterogeneity on horizontal heat conduction. Neglecting horizontal processes causes underestimating the conductive heat flux of 10% or more. Furthermore, comparing model results to independent temperature observations reveals a similar to 5 K surface temperature overestimation over ice thinner than 1 m, attributed to shortcomings in parameterizing surface turbulent and radiative fluxes rather than the conduction. Assessing the model deficiencies and parameterizing these unresolved processes is required for improved sea ice representation. 2138788 Article in Journal/Newspaper Arctic Sea ice OpenSky (NCAR/UCAR - National Center for Atmospheric Research/University Corporation for Atmospheric Research) Arctic Geophysical Research Letters 51 8
institution Open Polar
collection OpenSky (NCAR/UCAR - National Center for Atmospheric Research/University Corporation for Atmospheric Research)
op_collection_id ftncar
language English
description Models struggle to accurately simulate observed sea ice thickness changes, which could be partially due to inadequate representation of thermodynamic processes. We analyzed co-located winter observations of the Arctic sea ice from the Multidisciplinary Drifting Observatory for the Study of the Arctic Climate for evaluating and improving thermodynamic processes in sea ice models, aiming to enable more accurate predictions of the warming climate system. We model the sea ice and snow heat conduction for observed transects forced by realistic boundary conditions to understand the impact of the non-resolved meter-scale snow and sea ice thickness heterogeneity on horizontal heat conduction. Neglecting horizontal processes causes underestimating the conductive heat flux of 10% or more. Furthermore, comparing model results to independent temperature observations reveals a similar to 5 K surface temperature overestimation over ice thinner than 1 m, attributed to shortcomings in parameterizing surface turbulent and radiative fluxes rather than the conduction. Assessing the model deficiencies and parameterizing these unresolved processes is required for improved sea ice representation. 2138788
author2 Zampieri, Lorenzo (author)
Clemens‐Sewall, David (author)
Sledd, Anne (author)
Hutter, Nils (author)
Holland, Marika (author)
format Article in Journal/Newspaper
title Modeling the winter heat conduction through the sea ice system during MOSAiC
spellingShingle Modeling the winter heat conduction through the sea ice system during MOSAiC
title_short Modeling the winter heat conduction through the sea ice system during MOSAiC
title_full Modeling the winter heat conduction through the sea ice system during MOSAiC
title_fullStr Modeling the winter heat conduction through the sea ice system during MOSAiC
title_full_unstemmed Modeling the winter heat conduction through the sea ice system during MOSAiC
title_sort modeling the winter heat conduction through the sea ice system during mosaic
publishDate 2024
url https://doi.org/10.1029/2023GL106760
geographic Arctic
geographic_facet Arctic
genre Arctic
Sea ice
genre_facet Arctic
Sea ice
op_relation Geophysical Research Letters--Geophysical Research Letters--0094-8276--1944-8007
articles:27163
doi:10.1029/2023GL106760
ark:/85065/d7sx6jdv
op_rights Copyright author(s). This work is licensed under a Creative Commons Attribution-NonCommercial 4.0 International License.
op_doi https://doi.org/10.1029/2023GL106760
container_title Geophysical Research Letters
container_volume 51
container_issue 8
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