Deliverable No. 4.5 Interim evaluation of initialization experiments investigating the impact of novel observations in the coupled atmosphere–land–ocean–sea ice system

Initial-value information is a key source of polar predictability at sub-seasonal to seasonal time scales. However, how to constrain numerical models with actual observations at initial prediction time is a technical and scientific challenge. The observational network is sparse and not all physicall...

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Main Author: Massonnet, François
Format: Report
Language:English
Published: Zenodo 2018
Subjects:
Online Access:https://doi.org/10.5281/zenodo.3569282
id ftzenodo:oai:zenodo.org:3569282
record_format openpolar
spelling ftzenodo:oai:zenodo.org:3569282 2024-09-15T18:23:51+00:00 Deliverable No. 4.5 Interim evaluation of initialization experiments investigating the impact of novel observations in the coupled atmosphere–land–ocean–sea ice system Massonnet, François 2018-10-23 https://doi.org/10.5281/zenodo.3569282 eng eng Zenodo https://zenodo.org/communities/eu https://doi.org/10.5281/zenodo.3569281 https://doi.org/10.5281/zenodo.3569282 oai:zenodo.org:3569282 info:eu-repo/semantics/openAccess Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode info:eu-repo/semantics/report 2018 ftzenodo https://doi.org/10.5281/zenodo.356928210.5281/zenodo.3569281 2024-07-25T20:36:18Z Initial-value information is a key source of polar predictability at sub-seasonal to seasonal time scales. However, how to constrain numerical models with actual observations at initial prediction time is a technical and scientific challenge. The observational network is sparse and not all physically relevant variables for initialization are well monitored. In addition, numerical models used in predictions have their own biases, which introduces numerical instabilities and shocks after initialization. One objective of APPLICATE WP4 is to deliver recommendations for optimal initialization strategies of weather and climate models. In this “interim” deliverable, progress is presented on the initialization of novel products and on the use of novel assimilation techniques. It is found that sea ice initialization can benefit the skill in the North Atlantic Oscillation (NAO) prediction, but that sea ice has to be initialized in a consistent way with the ocean underneath to avoid initial shocks. In retrospective seasonal prediction experiments, initialization of sea ice thickness gives promising results for forecasting the summer sea ice edge position, a diagnostic of interest for a wide range of stakeholders. Finally, a new scheme has been developed for assimilation of continental snow in a multi-layer model, opening prospects for enhanced land-surface- induced predictability at sub-seasonal time scales. The work summarized in this deliverable is still ongoing, will be continued until the end of the project, and will result in further recommendations for optimal initialization techniques to be applied in WP5. Report North Atlantic North Atlantic oscillation Sea ice Zenodo
institution Open Polar
collection Zenodo
op_collection_id ftzenodo
language English
description Initial-value information is a key source of polar predictability at sub-seasonal to seasonal time scales. However, how to constrain numerical models with actual observations at initial prediction time is a technical and scientific challenge. The observational network is sparse and not all physically relevant variables for initialization are well monitored. In addition, numerical models used in predictions have their own biases, which introduces numerical instabilities and shocks after initialization. One objective of APPLICATE WP4 is to deliver recommendations for optimal initialization strategies of weather and climate models. In this “interim” deliverable, progress is presented on the initialization of novel products and on the use of novel assimilation techniques. It is found that sea ice initialization can benefit the skill in the North Atlantic Oscillation (NAO) prediction, but that sea ice has to be initialized in a consistent way with the ocean underneath to avoid initial shocks. In retrospective seasonal prediction experiments, initialization of sea ice thickness gives promising results for forecasting the summer sea ice edge position, a diagnostic of interest for a wide range of stakeholders. Finally, a new scheme has been developed for assimilation of continental snow in a multi-layer model, opening prospects for enhanced land-surface- induced predictability at sub-seasonal time scales. The work summarized in this deliverable is still ongoing, will be continued until the end of the project, and will result in further recommendations for optimal initialization techniques to be applied in WP5.
format Report
author Massonnet, François
spellingShingle Massonnet, François
Deliverable No. 4.5 Interim evaluation of initialization experiments investigating the impact of novel observations in the coupled atmosphere–land–ocean–sea ice system
author_facet Massonnet, François
author_sort Massonnet, François
title Deliverable No. 4.5 Interim evaluation of initialization experiments investigating the impact of novel observations in the coupled atmosphere–land–ocean–sea ice system
title_short Deliverable No. 4.5 Interim evaluation of initialization experiments investigating the impact of novel observations in the coupled atmosphere–land–ocean–sea ice system
title_full Deliverable No. 4.5 Interim evaluation of initialization experiments investigating the impact of novel observations in the coupled atmosphere–land–ocean–sea ice system
title_fullStr Deliverable No. 4.5 Interim evaluation of initialization experiments investigating the impact of novel observations in the coupled atmosphere–land–ocean–sea ice system
title_full_unstemmed Deliverable No. 4.5 Interim evaluation of initialization experiments investigating the impact of novel observations in the coupled atmosphere–land–ocean–sea ice system
title_sort deliverable no. 4.5 interim evaluation of initialization experiments investigating the impact of novel observations in the coupled atmosphere–land–ocean–sea ice system
publisher Zenodo
publishDate 2018
url https://doi.org/10.5281/zenodo.3569282
genre North Atlantic
North Atlantic oscillation
Sea ice
genre_facet North Atlantic
North Atlantic oscillation
Sea ice
op_relation https://zenodo.org/communities/eu
https://doi.org/10.5281/zenodo.3569281
https://doi.org/10.5281/zenodo.3569282
oai:zenodo.org:3569282
op_rights info:eu-repo/semantics/openAccess
Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
op_doi https://doi.org/10.5281/zenodo.356928210.5281/zenodo.3569281
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