Deliverable 6.4 Ice-ocean statistics and state estimation V1

Based on a coupled ocean-sea ice model and its adjoint model, we evaluate the capacity of the existing Arctic Ocean observing system on capturing different aspects of the Arctic Ocean changes, using Observing System Simulation Experiments (OSSEs). Subsequently, we produce a 10-year ocean-sea ice syn...

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Main Authors: Lyu, Guokun, Serra, Nuna, Koehl, Armin, Stammer, Detlef
Format: Report
Language:English
Published: 2020
Subjects:
Online Access:https://zenodo.org/record/7137504
https://doi.org/10.5281/zenodo.7137504
id ftzenodo:oai:zenodo.org:7137504
record_format openpolar
spelling ftzenodo:oai:zenodo.org:7137504 2023-05-15T14:46:36+02:00 Deliverable 6.4 Ice-ocean statistics and state estimation V1 Lyu, Guokun Serra, Nuna Koehl, Armin Stammer, Detlef 2020-02-04 https://zenodo.org/record/7137504 https://doi.org/10.5281/zenodo.7137504 eng eng info:eu-repo/grantAgreement/EC/H2020/727890/ doi:10.5281/zenodo.7137503 https://zenodo.org/communities/intaros-h2020 https://zenodo.org/record/7137504 https://doi.org/10.5281/zenodo.7137504 oai:zenodo.org:7137504 info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by/4.0/legalcode Arctic INTAROS Observing System Simulation Experiment Observing Systems Ocean Observing Systems Sea Ice Observing Systems Model In Situ Data Sea Ice Concentration info:eu-repo/semantics/report publication-deliverable 2020 ftzenodo https://doi.org/10.5281/zenodo.713750410.5281/zenodo.7137503 2023-03-10T13:45:16Z Based on a coupled ocean-sea ice model and its adjoint model, we evaluate the capacity of the existing Arctic Ocean observing system on capturing different aspects of the Arctic Ocean changes, using Observing System Simulation Experiments (OSSEs). Subsequently, we produce a 10-year ocean-sea ice synthesis by assimilating all available observations into the system. The main findings are: 1) Moorings deployed in the Fram Strait and along the pathway of Atlantic inflow to the Arctic Ocean are critical to capture the remote-propagating signals. The existing mooring system needs to be enhanced. 2) Sea ice processes, especially sea ice concentration changes, are the dominant mode that is improved by data assimilation. The improvement benefits from the spatiotemporal coverage of sea ice concentration observations. 3) Changes in the temperature and salinity are tiny in the ice-covered region and are caused by enhanced air-sea interaction due to sea ice reduction. Although the availability of hydrographic profiles increased significantly over the past decades, its effects are not apparent in the data assimilation experiments. Report Arctic Arctic Ocean Fram Strait Sea ice Zenodo Arctic Arctic Ocean
institution Open Polar
collection Zenodo
op_collection_id ftzenodo
language English
topic Arctic
INTAROS
Observing System Simulation Experiment
Observing Systems
Ocean Observing Systems
Sea Ice Observing Systems
Model
In Situ Data
Sea Ice Concentration
spellingShingle Arctic
INTAROS
Observing System Simulation Experiment
Observing Systems
Ocean Observing Systems
Sea Ice Observing Systems
Model
In Situ Data
Sea Ice Concentration
Lyu, Guokun
Serra, Nuna
Koehl, Armin
Stammer, Detlef
Deliverable 6.4 Ice-ocean statistics and state estimation V1
topic_facet Arctic
INTAROS
Observing System Simulation Experiment
Observing Systems
Ocean Observing Systems
Sea Ice Observing Systems
Model
In Situ Data
Sea Ice Concentration
description Based on a coupled ocean-sea ice model and its adjoint model, we evaluate the capacity of the existing Arctic Ocean observing system on capturing different aspects of the Arctic Ocean changes, using Observing System Simulation Experiments (OSSEs). Subsequently, we produce a 10-year ocean-sea ice synthesis by assimilating all available observations into the system. The main findings are: 1) Moorings deployed in the Fram Strait and along the pathway of Atlantic inflow to the Arctic Ocean are critical to capture the remote-propagating signals. The existing mooring system needs to be enhanced. 2) Sea ice processes, especially sea ice concentration changes, are the dominant mode that is improved by data assimilation. The improvement benefits from the spatiotemporal coverage of sea ice concentration observations. 3) Changes in the temperature and salinity are tiny in the ice-covered region and are caused by enhanced air-sea interaction due to sea ice reduction. Although the availability of hydrographic profiles increased significantly over the past decades, its effects are not apparent in the data assimilation experiments.
format Report
author Lyu, Guokun
Serra, Nuna
Koehl, Armin
Stammer, Detlef
author_facet Lyu, Guokun
Serra, Nuna
Koehl, Armin
Stammer, Detlef
author_sort Lyu, Guokun
title Deliverable 6.4 Ice-ocean statistics and state estimation V1
title_short Deliverable 6.4 Ice-ocean statistics and state estimation V1
title_full Deliverable 6.4 Ice-ocean statistics and state estimation V1
title_fullStr Deliverable 6.4 Ice-ocean statistics and state estimation V1
title_full_unstemmed Deliverable 6.4 Ice-ocean statistics and state estimation V1
title_sort deliverable 6.4 ice-ocean statistics and state estimation v1
publishDate 2020
url https://zenodo.org/record/7137504
https://doi.org/10.5281/zenodo.7137504
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre Arctic
Arctic Ocean
Fram Strait
Sea ice
genre_facet Arctic
Arctic Ocean
Fram Strait
Sea ice
op_relation info:eu-repo/grantAgreement/EC/H2020/727890/
doi:10.5281/zenodo.7137503
https://zenodo.org/communities/intaros-h2020
https://zenodo.org/record/7137504
https://doi.org/10.5281/zenodo.7137504
oai:zenodo.org:7137504
op_rights info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by/4.0/legalcode
op_doi https://doi.org/10.5281/zenodo.713750410.5281/zenodo.7137503
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