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...

Full description

Bibliographic Details
Published in:Oceans
Main Authors: Sukun Cheng, Ali Aydoğdu, Pierre Rampal, Alberto Carrassi, Laurent Bertino
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2020
Subjects:
Online Access:https://doi.org/10.3390/oceans1040022
id ftmdpi:oai:mdpi.com:/2673-1924/1/4/22/
record_format openpolar
spelling 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