Performance of a Coupled Arctic Climate Model Compared to MOSAiC Observations and its Sensitivity to a Change in Snow Thermal Conductivity ...

Climate models like the coupled Arctic atmosphere-ocean-sea ice model HIRHAM-NAOSIM are helpful to gain a deeper understanding of Arctic Amplification and interactions between atmosphere, ocean and sea ice. HIRHAM-NAOSIM is evaluated in Arctic winter compared to data from the MOSAiC expedition for F...

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Main Author: Röntgen, Leonie
Format: Text
Language:English
Published: Zenodo 2023
Subjects:
Online Access:https://dx.doi.org/10.5281/zenodo.7693669
https://zenodo.org/record/7693669
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spelling ftdatacite:10.5281/zenodo.7693669 2023-05-15T14:42:13+02:00 Performance of a Coupled Arctic Climate Model Compared to MOSAiC Observations and its Sensitivity to a Change in Snow Thermal Conductivity ... Röntgen, Leonie 2023 https://dx.doi.org/10.5281/zenodo.7693669 https://zenodo.org/record/7693669 en eng Zenodo https://dx.doi.org/10.5281/zenodo.7693668 Open Access Creative Commons Attribution 3.0 Germany https://creativecommons.org/licenses/by/3.0/de/legalcode info:eu-repo/semantics/openAccess Thesis ScholarlyArticle article-journal Text 2023 ftdatacite https://doi.org/10.5281/zenodo.769366910.5281/zenodo.7693668 2023-04-03T12:51:11Z Climate models like the coupled Arctic atmosphere-ocean-sea ice model HIRHAM-NAOSIM are helpful to gain a deeper understanding of Arctic Amplification and interactions between atmosphere, ocean and sea ice. HIRHAM-NAOSIM is evaluated in Arctic winter compared to data from the MOSAiC expedition for February 2020. A warm surface temperature bias of more than 5°C during clear-sky conditions is discussed in terms of modeled surface energy budget, clouds and atmospheric stability. HIRHAM-NAOSIM's control run underestimates the stable atmospheric stratification and has a positive bias in liquid water path and longwave radiation during observed clear-sky time periods. Though the positive longwave radiative bias outweighs the impact of a changed snow thermal conductivity and the positive temperature bias during radiatively clear state remains, a halved conductivity of 0.15 Wm -1 K -1 reduces the simulated surface temperature by up to 5°C and causes a higher occurrence of stable atmospheric conditions. ... Text Arctic Sea ice DataCite Metadata Store (German National Library of Science and Technology) Arctic
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
description Climate models like the coupled Arctic atmosphere-ocean-sea ice model HIRHAM-NAOSIM are helpful to gain a deeper understanding of Arctic Amplification and interactions between atmosphere, ocean and sea ice. HIRHAM-NAOSIM is evaluated in Arctic winter compared to data from the MOSAiC expedition for February 2020. A warm surface temperature bias of more than 5°C during clear-sky conditions is discussed in terms of modeled surface energy budget, clouds and atmospheric stability. HIRHAM-NAOSIM's control run underestimates the stable atmospheric stratification and has a positive bias in liquid water path and longwave radiation during observed clear-sky time periods. Though the positive longwave radiative bias outweighs the impact of a changed snow thermal conductivity and the positive temperature bias during radiatively clear state remains, a halved conductivity of 0.15 Wm -1 K -1 reduces the simulated surface temperature by up to 5°C and causes a higher occurrence of stable atmospheric conditions. ...
format Text
author Röntgen, Leonie
spellingShingle Röntgen, Leonie
Performance of a Coupled Arctic Climate Model Compared to MOSAiC Observations and its Sensitivity to a Change in Snow Thermal Conductivity ...
author_facet Röntgen, Leonie
author_sort Röntgen, Leonie
title Performance of a Coupled Arctic Climate Model Compared to MOSAiC Observations and its Sensitivity to a Change in Snow Thermal Conductivity ...
title_short Performance of a Coupled Arctic Climate Model Compared to MOSAiC Observations and its Sensitivity to a Change in Snow Thermal Conductivity ...
title_full Performance of a Coupled Arctic Climate Model Compared to MOSAiC Observations and its Sensitivity to a Change in Snow Thermal Conductivity ...
title_fullStr Performance of a Coupled Arctic Climate Model Compared to MOSAiC Observations and its Sensitivity to a Change in Snow Thermal Conductivity ...
title_full_unstemmed Performance of a Coupled Arctic Climate Model Compared to MOSAiC Observations and its Sensitivity to a Change in Snow Thermal Conductivity ...
title_sort performance of a coupled arctic climate model compared to mosaic observations and its sensitivity to a change in snow thermal conductivity ...
publisher Zenodo
publishDate 2023
url https://dx.doi.org/10.5281/zenodo.7693669
https://zenodo.org/record/7693669
geographic Arctic
geographic_facet Arctic
genre Arctic
Sea ice
genre_facet Arctic
Sea ice
op_relation https://dx.doi.org/10.5281/zenodo.7693668
op_rights Open Access
Creative Commons Attribution 3.0 Germany
https://creativecommons.org/licenses/by/3.0/de/legalcode
info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.5281/zenodo.769366910.5281/zenodo.7693668
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