The influence of a daily-updating sea ice on Antarctic and Southern Ocean numerical weather prediction

Although operational weather forecasting centres are increasingly using global coupled atmosphere-ocean-ice models to replace atmosphere-only models for short- and medium-range (10-day) weather forecasting, the influence of sea ice on such forecasting has yet to be fully quantified, especially in th...

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Main Authors: Zhaohui Wang, Alexander D. Fraser, Phil Reid, Richard Coleman, Siobhan O'Farrell
Format: Article in Journal/Newspaper
Language:unknown
Published: 2023
Subjects:
Online Access:https://zenodo.org/record/8017740
https://doi.org/10.5281/zenodo.8017740
id ftzenodo:oai:zenodo.org:8017740
record_format openpolar
spelling ftzenodo:oai:zenodo.org:8017740 2023-07-02T03:30:01+02:00 The influence of a daily-updating sea ice on Antarctic and Southern Ocean numerical weather prediction Zhaohui Wang Alexander D. Fraser Phil Reid Richard Coleman Siobhan O'Farrell 2023-06-08 https://zenodo.org/record/8017740 https://doi.org/10.5281/zenodo.8017740 unknown doi:10.5281/zenodo.8017739 https://zenodo.org/record/8017740 https://doi.org/10.5281/zenodo.8017740 oai:zenodo.org:8017740 info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by/4.0/legalcode Antarctic sea ice Numerical Weather Prediction info:eu-repo/semantics/article publication-article 2023 ftzenodo https://doi.org/10.5281/zenodo.801774010.5281/zenodo.8017739 2023-06-13T22:58:02Z Although operational weather forecasting centres are increasingly using global coupled atmosphere-ocean-ice models to replace atmosphere-only models for short- and medium-range (10-day) weather forecasting, the influence of sea ice on such forecasting has yet to be fully quantified, especially in the Southern Ocean. To address this gap, a polar-specific version of the Weather Research and Forecasting model is implemented with a circumpolar Antarctic domain to investigate the impact of daily updates of sea-ice concentration on short- and medium- range weather forecasting. A statistically-significant improvement in near-surface atmospheric temperature and humidity is shown from +48 hours to +192 hours when updating the daily sea-ice concentration in the model. The forecast skill improvements for 2 m temperature and dewpoint temperature are enhanced from July to September, which is the period of late sea-ice advance. Regionally, model improvement is shown to occur in most sea-ice regions, although the improvement is strongest in the Ross Sea and Weddell Sea sectors. The surface heat budget also shows remarkable improvement in outgoing radiative heat fluxes and both sensible and latent heat fluxes after 48 hours. This idealised research demonstrates the non-negligible effect of including more accurate sea-ice concentration in numerical weather forecasting. Article in Journal/Newspaper Antarc* Antarctic Ross Sea Sea ice Southern Ocean Weddell Sea Zenodo Antarctic Ross Sea Southern Ocean Weddell Weddell Sea
institution Open Polar
collection Zenodo
op_collection_id ftzenodo
language unknown
topic Antarctic sea ice
Numerical Weather Prediction
spellingShingle Antarctic sea ice
Numerical Weather Prediction
Zhaohui Wang
Alexander D. Fraser
Phil Reid
Richard Coleman
Siobhan O'Farrell
The influence of a daily-updating sea ice on Antarctic and Southern Ocean numerical weather prediction
topic_facet Antarctic sea ice
Numerical Weather Prediction
description Although operational weather forecasting centres are increasingly using global coupled atmosphere-ocean-ice models to replace atmosphere-only models for short- and medium-range (10-day) weather forecasting, the influence of sea ice on such forecasting has yet to be fully quantified, especially in the Southern Ocean. To address this gap, a polar-specific version of the Weather Research and Forecasting model is implemented with a circumpolar Antarctic domain to investigate the impact of daily updates of sea-ice concentration on short- and medium- range weather forecasting. A statistically-significant improvement in near-surface atmospheric temperature and humidity is shown from +48 hours to +192 hours when updating the daily sea-ice concentration in the model. The forecast skill improvements for 2 m temperature and dewpoint temperature are enhanced from July to September, which is the period of late sea-ice advance. Regionally, model improvement is shown to occur in most sea-ice regions, although the improvement is strongest in the Ross Sea and Weddell Sea sectors. The surface heat budget also shows remarkable improvement in outgoing radiative heat fluxes and both sensible and latent heat fluxes after 48 hours. This idealised research demonstrates the non-negligible effect of including more accurate sea-ice concentration in numerical weather forecasting.
format Article in Journal/Newspaper
author Zhaohui Wang
Alexander D. Fraser
Phil Reid
Richard Coleman
Siobhan O'Farrell
author_facet Zhaohui Wang
Alexander D. Fraser
Phil Reid
Richard Coleman
Siobhan O'Farrell
author_sort Zhaohui Wang
title The influence of a daily-updating sea ice on Antarctic and Southern Ocean numerical weather prediction
title_short The influence of a daily-updating sea ice on Antarctic and Southern Ocean numerical weather prediction
title_full The influence of a daily-updating sea ice on Antarctic and Southern Ocean numerical weather prediction
title_fullStr The influence of a daily-updating sea ice on Antarctic and Southern Ocean numerical weather prediction
title_full_unstemmed The influence of a daily-updating sea ice on Antarctic and Southern Ocean numerical weather prediction
title_sort influence of a daily-updating sea ice on antarctic and southern ocean numerical weather prediction
publishDate 2023
url https://zenodo.org/record/8017740
https://doi.org/10.5281/zenodo.8017740
geographic Antarctic
Ross Sea
Southern Ocean
Weddell
Weddell Sea
geographic_facet Antarctic
Ross Sea
Southern Ocean
Weddell
Weddell Sea
genre Antarc*
Antarctic
Ross Sea
Sea ice
Southern Ocean
Weddell Sea
genre_facet Antarc*
Antarctic
Ross Sea
Sea ice
Southern Ocean
Weddell Sea
op_relation doi:10.5281/zenodo.8017739
https://zenodo.org/record/8017740
https://doi.org/10.5281/zenodo.8017740
oai:zenodo.org:8017740
op_rights info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by/4.0/legalcode
op_doi https://doi.org/10.5281/zenodo.801774010.5281/zenodo.8017739
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