Edge displacement scores

As a consequence of a diminishing sea ice cover in the Arctic, activity is on the rise. The position of the sea ice edge, which is generally taken to define the extent of the ice cover, changes in response to dynamic and thermodynamic processes. Forecasts for sea ice expansion due to an advancing ic...

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Main Author: Melsom, Arne
Format: Text
Language:English
Published: 2021
Subjects:
Online Access:https://doi.org/10.5194/tc-2020-361
https://tc.copernicus.org/preprints/tc-2020-361/
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spelling ftcopernicus:oai:publications.copernicus.org:tcd91793 2023-05-15T15:01:03+02:00 Edge displacement scores Melsom, Arne 2021-02-18 application/pdf https://doi.org/10.5194/tc-2020-361 https://tc.copernicus.org/preprints/tc-2020-361/ eng eng doi:10.5194/tc-2020-361 https://tc.copernicus.org/preprints/tc-2020-361/ eISSN: 1994-0424 Text 2021 ftcopernicus https://doi.org/10.5194/tc-2020-361 2021-02-22T17:22:14Z As a consequence of a diminishing sea ice cover in the Arctic, activity is on the rise. The position of the sea ice edge, which is generally taken to define the extent of the ice cover, changes in response to dynamic and thermodynamic processes. Forecasts for sea ice expansion due to an advancing ice edge will provide information that can be of significance for operations in polar regions. However, the value of this information depends on the quality of the forecasts. Here, we present methods for examining the quality of forecasted sea ice expansion and the geographic location where the largest expansion are expected from the forecast results. The algorithm is simple to implement, and an examination of two years of model results and accompanying observations demonstrates the usefulness of the analysis. Text Arctic Sea ice Copernicus Publications: E-Journals Arctic
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description As a consequence of a diminishing sea ice cover in the Arctic, activity is on the rise. The position of the sea ice edge, which is generally taken to define the extent of the ice cover, changes in response to dynamic and thermodynamic processes. Forecasts for sea ice expansion due to an advancing ice edge will provide information that can be of significance for operations in polar regions. However, the value of this information depends on the quality of the forecasts. Here, we present methods for examining the quality of forecasted sea ice expansion and the geographic location where the largest expansion are expected from the forecast results. The algorithm is simple to implement, and an examination of two years of model results and accompanying observations demonstrates the usefulness of the analysis.
format Text
author Melsom, Arne
spellingShingle Melsom, Arne
Edge displacement scores
author_facet Melsom, Arne
author_sort Melsom, Arne
title Edge displacement scores
title_short Edge displacement scores
title_full Edge displacement scores
title_fullStr Edge displacement scores
title_full_unstemmed Edge displacement scores
title_sort edge displacement scores
publishDate 2021
url https://doi.org/10.5194/tc-2020-361
https://tc.copernicus.org/preprints/tc-2020-361/
geographic Arctic
geographic_facet Arctic
genre Arctic
Sea ice
genre_facet Arctic
Sea ice
op_source eISSN: 1994-0424
op_relation doi:10.5194/tc-2020-361
https://tc.copernicus.org/preprints/tc-2020-361/
op_doi https://doi.org/10.5194/tc-2020-361
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