Trivial gain of downscaling in future projections of higher trophic levels in the Nordic and Barents Seas

Abstract Downscaling physical forcing from global climate models is both time consuming and labor demanding and can delay or limit the physical forcing available for regional marine ecosystem modelers. Earlier studies have shown that downscaled physics is necessary for capturing the dynamics of prim...

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Published in:Fisheries Oceanography
Main Authors: Nilsen, Ina, Fransner, Filippa, Olsen, Are, Tjiputra, Jerry, Hordoir, Robinson, Hansen, Cecilie
Other Authors: Norges Forskningsråd
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2023
Subjects:
Online Access:http://dx.doi.org/10.1111/fog.12641
https://onlinelibrary.wiley.com/doi/pdf/10.1111/fog.12641
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spelling crwiley:10.1111/fog.12641 2024-06-02T08:00:08+00:00 Trivial gain of downscaling in future projections of higher trophic levels in the Nordic and Barents Seas Nilsen, Ina Fransner, Filippa Olsen, Are Tjiputra, Jerry Hordoir, Robinson Hansen, Cecilie Norges Forskningsråd 2023 http://dx.doi.org/10.1111/fog.12641 https://onlinelibrary.wiley.com/doi/pdf/10.1111/fog.12641 en eng Wiley http://creativecommons.org/licenses/by/4.0/ Fisheries Oceanography volume 32, issue 5, page 479-493 ISSN 1054-6006 1365-2419 journal-article 2023 crwiley https://doi.org/10.1111/fog.12641 2024-05-03T10:59:16Z Abstract Downscaling physical forcing from global climate models is both time consuming and labor demanding and can delay or limit the physical forcing available for regional marine ecosystem modelers. Earlier studies have shown that downscaled physics is necessary for capturing the dynamics of primary production and lower trophic levels; however, it is not clear how higher trophic levels respond to the coarse resolution physics of global models. Here, we apply the Nordic and Barents Seas Atlantis ecosystem model (NoBa) to study the consequences of using physical forcing from global climate models versus using that from regional models. The study is therefore (i) a comparison between a regional model and its driving global model to investigate the extent to which a global climate model can be used for regional ecosystem predictions and (ii) a study of the impact of future climate change in the Nordic and Barents Seas. We found that few higher trophic level species were affected by using forcing from a global versus a regional model, and there was a general agreement in future biomass trends and distribution patterns. However, the slight difference in temperature between the models dramatically impacted Northeast Arctic cod ( Gadus morhua ), which highlights how species projection uncertainty could arise from poor physical representation of the physical forcing, in addition to uncertainty in the ecosystem model parameterization. Article in Journal/Newspaper Arctic cod Arctic Climate change Gadus morhua Northeast Arctic cod Wiley Online Library Arctic Fisheries Oceanography 32 5 479 493
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract Downscaling physical forcing from global climate models is both time consuming and labor demanding and can delay or limit the physical forcing available for regional marine ecosystem modelers. Earlier studies have shown that downscaled physics is necessary for capturing the dynamics of primary production and lower trophic levels; however, it is not clear how higher trophic levels respond to the coarse resolution physics of global models. Here, we apply the Nordic and Barents Seas Atlantis ecosystem model (NoBa) to study the consequences of using physical forcing from global climate models versus using that from regional models. The study is therefore (i) a comparison between a regional model and its driving global model to investigate the extent to which a global climate model can be used for regional ecosystem predictions and (ii) a study of the impact of future climate change in the Nordic and Barents Seas. We found that few higher trophic level species were affected by using forcing from a global versus a regional model, and there was a general agreement in future biomass trends and distribution patterns. However, the slight difference in temperature between the models dramatically impacted Northeast Arctic cod ( Gadus morhua ), which highlights how species projection uncertainty could arise from poor physical representation of the physical forcing, in addition to uncertainty in the ecosystem model parameterization.
author2 Norges Forskningsråd
format Article in Journal/Newspaper
author Nilsen, Ina
Fransner, Filippa
Olsen, Are
Tjiputra, Jerry
Hordoir, Robinson
Hansen, Cecilie
spellingShingle Nilsen, Ina
Fransner, Filippa
Olsen, Are
Tjiputra, Jerry
Hordoir, Robinson
Hansen, Cecilie
Trivial gain of downscaling in future projections of higher trophic levels in the Nordic and Barents Seas
author_facet Nilsen, Ina
Fransner, Filippa
Olsen, Are
Tjiputra, Jerry
Hordoir, Robinson
Hansen, Cecilie
author_sort Nilsen, Ina
title Trivial gain of downscaling in future projections of higher trophic levels in the Nordic and Barents Seas
title_short Trivial gain of downscaling in future projections of higher trophic levels in the Nordic and Barents Seas
title_full Trivial gain of downscaling in future projections of higher trophic levels in the Nordic and Barents Seas
title_fullStr Trivial gain of downscaling in future projections of higher trophic levels in the Nordic and Barents Seas
title_full_unstemmed Trivial gain of downscaling in future projections of higher trophic levels in the Nordic and Barents Seas
title_sort trivial gain of downscaling in future projections of higher trophic levels in the nordic and barents seas
publisher Wiley
publishDate 2023
url http://dx.doi.org/10.1111/fog.12641
https://onlinelibrary.wiley.com/doi/pdf/10.1111/fog.12641
geographic Arctic
geographic_facet Arctic
genre Arctic cod
Arctic
Climate change
Gadus morhua
Northeast Arctic cod
genre_facet Arctic cod
Arctic
Climate change
Gadus morhua
Northeast Arctic cod
op_source Fisheries Oceanography
volume 32, issue 5, page 479-493
ISSN 1054-6006 1365-2419
op_rights http://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.1111/fog.12641
container_title Fisheries Oceanography
container_volume 32
container_issue 5
container_start_page 479
op_container_end_page 493
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