On the predictability of Arctic sea ice considering stratospheric information

Atmospheric circulation is one of the major drivers of Arctic sea ice and so, one of the key elements for its predictability. Most studies devoted to the atmosphere-sea ice coupling have so far only considered the effects of the troposphere. However, the low predictability of the polar tropospheric...

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Main Authors: Ayarzagüena, B., Casanova, C., Calvo, N.
Format: Conference Object
Language:English
Published: 2023
Subjects:
Online Access:https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018830
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spelling ftgfzpotsdam:oai:gfzpublic.gfz-potsdam.de:item_5018830 2023-10-01T03:53:09+02:00 On the predictability of Arctic sea ice considering stratospheric information Ayarzagüena, B. Casanova, C. Calvo, N. 2023 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018830 eng eng info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-2014 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018830 XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG) info:eu-repo/semantics/conferenceObject 2023 ftgfzpotsdam https://doi.org/10.57757/IUGG23-2014 2023-09-03T23:42:28Z Atmospheric circulation is one of the major drivers of Arctic sea ice and so, one of the key elements for its predictability. Most studies devoted to the atmosphere-sea ice coupling have so far only considered the effects of the troposphere. However, the low predictability of the polar tropospheric weather beyond two weeks hampers longer predictions of the sea ice. Further, changes in the stratosphere, such as sudden stratospheric warmings, have been found to affect surface conditions for up to several weeks, being the polar region one of the most affected areas. Thus, the consideration of the occurrence of these events may remarkably improve the predictability of the Arctic area. In this study, we aim to evaluate the predictive capacity of SSWs at sub-seasonal scale on Arctic sea ice concentration (SIC). To do so, we have used hindcast simulations of the sub-seasonal prediction model of the European Centre for Medium-Range Weather Forecasts (ECMWF) during the 20-year period of 1999-2018. Our results show that the model can reproduce the downward propagation of the stratospheric signal expected after an SSW event. It also simulates significant SIC anomalies after the occurrence of the downward-propagating SSWs. Finally, our results indicate an improvement in the prediction of Arctic sea ice after downward propagating SSWs compared to years without SSWs. 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 Atmospheric circulation is one of the major drivers of Arctic sea ice and so, one of the key elements for its predictability. Most studies devoted to the atmosphere-sea ice coupling have so far only considered the effects of the troposphere. However, the low predictability of the polar tropospheric weather beyond two weeks hampers longer predictions of the sea ice. Further, changes in the stratosphere, such as sudden stratospheric warmings, have been found to affect surface conditions for up to several weeks, being the polar region one of the most affected areas. Thus, the consideration of the occurrence of these events may remarkably improve the predictability of the Arctic area. In this study, we aim to evaluate the predictive capacity of SSWs at sub-seasonal scale on Arctic sea ice concentration (SIC). To do so, we have used hindcast simulations of the sub-seasonal prediction model of the European Centre for Medium-Range Weather Forecasts (ECMWF) during the 20-year period of 1999-2018. Our results show that the model can reproduce the downward propagation of the stratospheric signal expected after an SSW event. It also simulates significant SIC anomalies after the occurrence of the downward-propagating SSWs. Finally, our results indicate an improvement in the prediction of Arctic sea ice after downward propagating SSWs compared to years without SSWs.
format Conference Object
author Ayarzagüena, B.
Casanova, C.
Calvo, N.
spellingShingle Ayarzagüena, B.
Casanova, C.
Calvo, N.
On the predictability of Arctic sea ice considering stratospheric information
author_facet Ayarzagüena, B.
Casanova, C.
Calvo, N.
author_sort Ayarzagüena, B.
title On the predictability of Arctic sea ice considering stratospheric information
title_short On the predictability of Arctic sea ice considering stratospheric information
title_full On the predictability of Arctic sea ice considering stratospheric information
title_fullStr On the predictability of Arctic sea ice considering stratospheric information
title_full_unstemmed On the predictability of Arctic sea ice considering stratospheric information
title_sort on the predictability of arctic sea ice considering stratospheric information
publishDate 2023
url https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018830
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/IUGG23-2014
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018830
op_doi https://doi.org/10.57757/IUGG23-2014
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