Probabilistic Forecasts of Sea Ice Trajectories in the Arctic: Impact of Uncertainties in Surface Wind and Ice Cohesion
We study the response of the Lagrangian sea ice model neXtSIM to the uncertainty in sea surface wind and sea ice cohesion. The ice mechanics in neXtSIM are based on a brittle-like rheological framework. The study considers short-term ensemble forecasts of Arctic sea ice from January to April 2008. E...
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2020
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ftmdpi:oai:mdpi.com:/2673-1924/1/4/22/ 2023-08-20T04:03:50+02:00 Probabilistic Forecasts of Sea Ice Trajectories in the Arctic: Impact of Uncertainties in Surface Wind and Ice Cohesion Sukun Cheng Ali Aydoğdu Pierre Rampal Alberto Carrassi Laurent Bertino agris 2020-12-14 application/pdf https://doi.org/10.3390/oceans1040022 EN eng Multidisciplinary Digital Publishing Institute https://dx.doi.org/10.3390/oceans1040022 https://creativecommons.org/licenses/by/4.0/ Oceans; Volume 1; Issue 4; Pages: 326-342 Arctic sea ice drift neXtSIM ensemble forecasting wind perturbation ice cohesion perturbation Text 2020 ftmdpi https://doi.org/10.3390/oceans1040022 2023-08-01T00:39:47Z We study the response of the Lagrangian sea ice model neXtSIM to the uncertainty in sea surface wind and sea ice cohesion. The ice mechanics in neXtSIM are based on a brittle-like rheological framework. The study considers short-term ensemble forecasts of Arctic sea ice from January to April 2008. Ensembles are generated by perturbing the wind inputs and ice cohesion field both separately and jointly. The resulting uncertainty in the probabilistic forecasts is evaluated statistically based on the analysis of Lagrangian sea ice trajectories as sampled by virtual drifters seeded in the model to cover the Arctic Ocean and using metrics borrowed from the search-and-rescue literature. The comparison among the different ensembles indicates that wind perturbations dominate the forecast uncertainty (i.e., the absolute spread of the ensemble), while the inhomogeneities in the ice cohesion field significantly increase the degree of anisotropy in the spread—i.e., trajectories drift divergently in different directions. We suggest that in order to obtain enough uncertainties in a sea ice model with brittle-like rheologies, to predict sea ice drift and trajectories, one should consider using ensemble-based simulations where at least wind forcing and sea ice cohesion are perturbed. Text Arctic Arctic Ocean Sea ice MDPI Open Access Publishing Arctic Arctic Ocean Oceans 1 4 326 342 |
institution |
Open Polar |
collection |
MDPI Open Access Publishing |
op_collection_id |
ftmdpi |
language |
English |
topic |
Arctic sea ice drift neXtSIM ensemble forecasting wind perturbation ice cohesion perturbation |
spellingShingle |
Arctic sea ice drift neXtSIM ensemble forecasting wind perturbation ice cohesion perturbation Sukun Cheng Ali Aydoğdu Pierre Rampal Alberto Carrassi Laurent Bertino Probabilistic Forecasts of Sea Ice Trajectories in the Arctic: Impact of Uncertainties in Surface Wind and Ice Cohesion |
topic_facet |
Arctic sea ice drift neXtSIM ensemble forecasting wind perturbation ice cohesion perturbation |
description |
We study the response of the Lagrangian sea ice model neXtSIM to the uncertainty in sea surface wind and sea ice cohesion. The ice mechanics in neXtSIM are based on a brittle-like rheological framework. The study considers short-term ensemble forecasts of Arctic sea ice from January to April 2008. Ensembles are generated by perturbing the wind inputs and ice cohesion field both separately and jointly. The resulting uncertainty in the probabilistic forecasts is evaluated statistically based on the analysis of Lagrangian sea ice trajectories as sampled by virtual drifters seeded in the model to cover the Arctic Ocean and using metrics borrowed from the search-and-rescue literature. The comparison among the different ensembles indicates that wind perturbations dominate the forecast uncertainty (i.e., the absolute spread of the ensemble), while the inhomogeneities in the ice cohesion field significantly increase the degree of anisotropy in the spread—i.e., trajectories drift divergently in different directions. We suggest that in order to obtain enough uncertainties in a sea ice model with brittle-like rheologies, to predict sea ice drift and trajectories, one should consider using ensemble-based simulations where at least wind forcing and sea ice cohesion are perturbed. |
format |
Text |
author |
Sukun Cheng Ali Aydoğdu Pierre Rampal Alberto Carrassi Laurent Bertino |
author_facet |
Sukun Cheng Ali Aydoğdu Pierre Rampal Alberto Carrassi Laurent Bertino |
author_sort |
Sukun Cheng |
title |
Probabilistic Forecasts of Sea Ice Trajectories in the Arctic: Impact of Uncertainties in Surface Wind and Ice Cohesion |
title_short |
Probabilistic Forecasts of Sea Ice Trajectories in the Arctic: Impact of Uncertainties in Surface Wind and Ice Cohesion |
title_full |
Probabilistic Forecasts of Sea Ice Trajectories in the Arctic: Impact of Uncertainties in Surface Wind and Ice Cohesion |
title_fullStr |
Probabilistic Forecasts of Sea Ice Trajectories in the Arctic: Impact of Uncertainties in Surface Wind and Ice Cohesion |
title_full_unstemmed |
Probabilistic Forecasts of Sea Ice Trajectories in the Arctic: Impact of Uncertainties in Surface Wind and Ice Cohesion |
title_sort |
probabilistic forecasts of sea ice trajectories in the arctic: impact of uncertainties in surface wind and ice cohesion |
publisher |
Multidisciplinary Digital Publishing Institute |
publishDate |
2020 |
url |
https://doi.org/10.3390/oceans1040022 |
op_coverage |
agris |
geographic |
Arctic Arctic Ocean |
geographic_facet |
Arctic Arctic Ocean |
genre |
Arctic Arctic Ocean Sea ice |
genre_facet |
Arctic Arctic Ocean Sea ice |
op_source |
Oceans; Volume 1; Issue 4; Pages: 326-342 |
op_relation |
https://dx.doi.org/10.3390/oceans1040022 |
op_rights |
https://creativecommons.org/licenses/by/4.0/ |
op_doi |
https://doi.org/10.3390/oceans1040022 |
container_title |
Oceans |
container_volume |
1 |
container_issue |
4 |
container_start_page |
326 |
op_container_end_page |
342 |
_version_ |
1774714259747373056 |