Modeling pan-Arctic seasonal and interannual landfast sea ice thickness and snow depth between 1979 and 2021 ...

Landfast sea ice (LFSI) is sensitive to local climate change, making it an important component of the cryosphere system. In this study, the LFSI around the pan-Arctic domain was simulated from 1979 to 2021 using a well-validated snow and ice thermodynamic model (HIGHTSI) under the framework of the F...

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Main Authors: Wang, Zihan, Zhao, Jiechen, Cheng, Bin, Hui, Fengming, Su, Jie, Cheng, Xiao
Format: Text
Language:unknown
Published: Taylor & Francis 2024
Subjects:
Online Access:https://dx.doi.org/10.6084/m9.figshare.26309888
https://tandf.figshare.com/articles/journal_contribution/Modeling_pan-Arctic_seasonal_and_interannual_landfast_sea_ice_thickness_and_snow_depth_between_1979_and_2021/26309888
id ftdatacite:10.6084/m9.figshare.26309888
record_format openpolar
spelling ftdatacite:10.6084/m9.figshare.26309888 2024-09-15T18:02:12+00:00 Modeling pan-Arctic seasonal and interannual landfast sea ice thickness and snow depth between 1979 and 2021 ... Wang, Zihan Zhao, Jiechen Cheng, Bin Hui, Fengming Su, Jie Cheng, Xiao 2024 https://dx.doi.org/10.6084/m9.figshare.26309888 https://tandf.figshare.com/articles/journal_contribution/Modeling_pan-Arctic_seasonal_and_interannual_landfast_sea_ice_thickness_and_snow_depth_between_1979_and_2021/26309888 unknown Taylor & Francis https://dx.doi.org/10.1080/17538947.2024.2376253 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Environmental Sciences not elsewhere classified Ecology FOS Biological sciences Biological Sciences not elsewhere classified Text Journal contribution ScholarlyArticle article-journal 2024 ftdatacite https://doi.org/10.6084/m9.figshare.2630988810.1080/17538947.2024.2376253 2024-08-01T10:36:48Z Landfast sea ice (LFSI) is sensitive to local climate change, making it an important component of the cryosphere system. In this study, the LFSI around the pan-Arctic domain was simulated from 1979 to 2021 using a well-validated snow and ice thermodynamic model (HIGHTSI) under the framework of the Fast Ice Prediction System (FIPS), forced by the ERA5 reanalysis. The simulation results agree well with the in-situ observations in the Canadian Arctic, with a mean error of −0.06 ± 0.29 m for ice thickness and −0.04 ± 0.12 m for snow depth. A decrease of −2.8 ± 0.4 cm/10a in thickness and −16.2 ± 1.5 km 3 /a in volume for the Arctic LFSI was modeled during this period. There was significant spatial variability among the different domains, with the fastest decline found in the Vilkitsky Strait. The modeled snow depth shows large interannual and spatial variations, which was confirmed by other modeling results. The spatiotemporal variations in both air temperature and precipitation are the driving factors for the ... Text Climate change Sea ice DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language unknown
topic Environmental Sciences not elsewhere classified
Ecology
FOS Biological sciences
Biological Sciences not elsewhere classified
spellingShingle Environmental Sciences not elsewhere classified
Ecology
FOS Biological sciences
Biological Sciences not elsewhere classified
Wang, Zihan
Zhao, Jiechen
Cheng, Bin
Hui, Fengming
Su, Jie
Cheng, Xiao
Modeling pan-Arctic seasonal and interannual landfast sea ice thickness and snow depth between 1979 and 2021 ...
topic_facet Environmental Sciences not elsewhere classified
Ecology
FOS Biological sciences
Biological Sciences not elsewhere classified
description Landfast sea ice (LFSI) is sensitive to local climate change, making it an important component of the cryosphere system. In this study, the LFSI around the pan-Arctic domain was simulated from 1979 to 2021 using a well-validated snow and ice thermodynamic model (HIGHTSI) under the framework of the Fast Ice Prediction System (FIPS), forced by the ERA5 reanalysis. The simulation results agree well with the in-situ observations in the Canadian Arctic, with a mean error of −0.06 ± 0.29 m for ice thickness and −0.04 ± 0.12 m for snow depth. A decrease of −2.8 ± 0.4 cm/10a in thickness and −16.2 ± 1.5 km 3 /a in volume for the Arctic LFSI was modeled during this period. There was significant spatial variability among the different domains, with the fastest decline found in the Vilkitsky Strait. The modeled snow depth shows large interannual and spatial variations, which was confirmed by other modeling results. The spatiotemporal variations in both air temperature and precipitation are the driving factors for the ...
format Text
author Wang, Zihan
Zhao, Jiechen
Cheng, Bin
Hui, Fengming
Su, Jie
Cheng, Xiao
author_facet Wang, Zihan
Zhao, Jiechen
Cheng, Bin
Hui, Fengming
Su, Jie
Cheng, Xiao
author_sort Wang, Zihan
title Modeling pan-Arctic seasonal and interannual landfast sea ice thickness and snow depth between 1979 and 2021 ...
title_short Modeling pan-Arctic seasonal and interannual landfast sea ice thickness and snow depth between 1979 and 2021 ...
title_full Modeling pan-Arctic seasonal and interannual landfast sea ice thickness and snow depth between 1979 and 2021 ...
title_fullStr Modeling pan-Arctic seasonal and interannual landfast sea ice thickness and snow depth between 1979 and 2021 ...
title_full_unstemmed Modeling pan-Arctic seasonal and interannual landfast sea ice thickness and snow depth between 1979 and 2021 ...
title_sort modeling pan-arctic seasonal and interannual landfast sea ice thickness and snow depth between 1979 and 2021 ...
publisher Taylor & Francis
publishDate 2024
url https://dx.doi.org/10.6084/m9.figshare.26309888
https://tandf.figshare.com/articles/journal_contribution/Modeling_pan-Arctic_seasonal_and_interannual_landfast_sea_ice_thickness_and_snow_depth_between_1979_and_2021/26309888
genre Climate change
Sea ice
genre_facet Climate change
Sea ice
op_relation https://dx.doi.org/10.1080/17538947.2024.2376253
op_rights Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_doi https://doi.org/10.6084/m9.figshare.2630988810.1080/17538947.2024.2376253
_version_ 1810439605136130048