Assessment of sub-seasonal to intra-annual sea ice forecast in the regional arctic system model

The rate of warming in the Arctic has been much faster than the global average and the decline of sea ice decline has been accelerated. The “low-ice regime” in the future is likely to happen and impacts the Arctic environment, especially around the Arctic coasts. Hence, it is becoming increasingly c...

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Main Authors: Lee, Y., Maslowski, W., Craig, A., Clement Kinney, J., Osinski, R.
Format: Conference Object
Language:English
Published: 2023
Subjects:
Online Access:https://gfzpublic.gfz-potsdam.de/pubman/item/item_5021147
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spelling ftgfzpotsdam:oai:gfzpublic.gfz-potsdam.de:item_5021147 2023-07-30T04:00:25+02:00 Assessment of sub-seasonal to intra-annual sea ice forecast in the regional arctic system model Lee, Y. Maslowski, W. Craig, A. Clement Kinney, J. Osinski, R. 2023-07-11 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5021147 eng eng info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-4739 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5021147 XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG) info:eu-repo/semantics/conferenceObject 2023 ftgfzpotsdam https://doi.org/10.57757/IUGG23-4739 2023-07-16T23:40:25Z The rate of warming in the Arctic has been much faster than the global average and the decline of sea ice decline has been accelerated. The “low-ice regime” in the future is likely to happen and impacts the Arctic environment, especially around the Arctic coasts. Hence, it is becoming increasingly critical to foresee changes in Arctic sea ice and climate states as well as their potential impacts to guide human activities from natural resource management to risk assessment decisions. While climate models project a continuous decline of sea ice on a decadal time scale, the advancement of reliable predictive skills in seasonal sea ice forecasts remains challenging. Here, we use a state-of-the-art numerical model, Regional Arctic System Model (RASM), which forecasts Arctic sea ice at time scales from weeks up to six months. RASM is a fully-coupled regional climate system model, consisting of the atmosphere, ocean, sea ice, and land components, coupled through the Community Earth System Model flux coupler. The ocean and sea ice configurations include the horizontal resolution of 1/12 degree with 45-vertical levels and 5-thickness categories, respectively. The atmosphere is configured on a 50-km grid with 40 vertical levels and dynamically downscaled using the Climate Forecasting System (CFS) Reanalysis (CFSR) and its version 2 (CFSv2). This presentation summarizes our results of summer sea ice predictions from 2011 to 2022. In particular, the effects of lead time and initial conditions are investigated on the quantitative skill of seasonal predictability of Arctic sea ice. Conference Object Arctic Sea ice GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam) Arctic
institution Open Polar
collection GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam)
op_collection_id ftgfzpotsdam
language English
description The rate of warming in the Arctic has been much faster than the global average and the decline of sea ice decline has been accelerated. The “low-ice regime” in the future is likely to happen and impacts the Arctic environment, especially around the Arctic coasts. Hence, it is becoming increasingly critical to foresee changes in Arctic sea ice and climate states as well as their potential impacts to guide human activities from natural resource management to risk assessment decisions. While climate models project a continuous decline of sea ice on a decadal time scale, the advancement of reliable predictive skills in seasonal sea ice forecasts remains challenging. Here, we use a state-of-the-art numerical model, Regional Arctic System Model (RASM), which forecasts Arctic sea ice at time scales from weeks up to six months. RASM is a fully-coupled regional climate system model, consisting of the atmosphere, ocean, sea ice, and land components, coupled through the Community Earth System Model flux coupler. The ocean and sea ice configurations include the horizontal resolution of 1/12 degree with 45-vertical levels and 5-thickness categories, respectively. The atmosphere is configured on a 50-km grid with 40 vertical levels and dynamically downscaled using the Climate Forecasting System (CFS) Reanalysis (CFSR) and its version 2 (CFSv2). This presentation summarizes our results of summer sea ice predictions from 2011 to 2022. In particular, the effects of lead time and initial conditions are investigated on the quantitative skill of seasonal predictability of Arctic sea ice.
format Conference Object
author Lee, Y.
Maslowski, W.
Craig, A.
Clement Kinney, J.
Osinski, R.
spellingShingle Lee, Y.
Maslowski, W.
Craig, A.
Clement Kinney, J.
Osinski, R.
Assessment of sub-seasonal to intra-annual sea ice forecast in the regional arctic system model
author_facet Lee, Y.
Maslowski, W.
Craig, A.
Clement Kinney, J.
Osinski, R.
author_sort Lee, Y.
title Assessment of sub-seasonal to intra-annual sea ice forecast in the regional arctic system model
title_short Assessment of sub-seasonal to intra-annual sea ice forecast in the regional arctic system model
title_full Assessment of sub-seasonal to intra-annual sea ice forecast in the regional arctic system model
title_fullStr Assessment of sub-seasonal to intra-annual sea ice forecast in the regional arctic system model
title_full_unstemmed Assessment of sub-seasonal to intra-annual sea ice forecast in the regional arctic system model
title_sort assessment of sub-seasonal to intra-annual sea ice forecast in the regional arctic system model
publishDate 2023
url https://gfzpublic.gfz-potsdam.de/pubman/item/item_5021147
geographic Arctic
geographic_facet Arctic
genre Arctic
Sea ice
genre_facet Arctic
Sea ice
op_source XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
op_relation info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-4739
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5021147
op_doi https://doi.org/10.57757/IUGG23-4739
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