The ocean mesoscale in a warming world: insights from multiscale modeling
State-of-the-art climate models and computing infrastructure are now able to resolve mesoscale ocean eddy activity in many contexts. However, in computationally intensive model applications, such as the Coupled Model Intercomparison Project (CMIP) or simulations of the high latitudes, grid resolutio...
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ftsubbremen:oai:media.suub.uni-bremen.de:Publications/elib/7964 2024-06-23T07:46:57+00:00 The ocean mesoscale in a warming world: insights from multiscale modeling Beech, Nathan Jung, Thomas Kanzow, Torsten 2024-05-24 application/pdf https://media.suub.uni-bremen.de/handle/elib/7964 https://doi.org/10.26092/elib/3010 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib79642 eng eng Universität Bremen Fachbereich 01: Physik/Elektrotechnik (FB 01) https://media.suub.uni-bremen.de/handle/elib/7964 https://doi.org/10.26092/elib/3010 doi:10.26092/elib/3010 urn:nbn:de:gbv:46-elib79642 info:eu-repo/semantics/openAccess CC BY 4.0 (Attribution) https://creativecommons.org/licenses/by/4.0/ ocean modelling ocean circulation climate change climate modeling oceanography 530 530 Physics ddc:530 Dissertation doctoralThesis 2024 ftsubbremen https://doi.org/10.26092/elib/3010 2024-06-12T01:24:39Z State-of-the-art climate models and computing infrastructure are now able to resolve mesoscale ocean eddy activity in many contexts. However, in computationally intensive model applications, such as the Coupled Model Intercomparison Project (CMIP) or simulations of the high latitudes, grid resolutions largely remain eddy-parameterizing due to resource constraints. These missing mesoscale processes are understood to be crucial drivers of ocean circulation and climate and may become still more relevant in the context of anthropogenic climate change. To overcome the computational limitations of traditional models, multiscale modeling strategies have been developed which can distribute grid resolution and resources based on resolution requirements and research goals. Here, several strategies for resolving the mesoscale using multiscale methods are described and the results of their implementation with the Finite volumE Sea ice Ocean Model (FESOM) are reported. In the first application, FESOM participates in CMIP6 with the strategy of concentrating computational resources on the major eddy-rich regions of the ocean. The resulting simulations are able to reproduce between 51 and 82% of observed eddy kinetic energy (EKE) in each region and project substantial climate change impacts on mesoscale activity for the first time at such a scale. The results include a poleward shift of eddy activity in most western boundary currents; EKE intensification in the Antarctic Circumpolar Current (ACC), Brazil and Malvinas Currents, and Kuroshio Current; EKE decline in the Gulf Stream; and intensification of Agulhas leakage. In a second application, FESOM is used to concentrate computational resources in the Southern Ocean and cost-reducing modeling strategies are used to enable fully eddy-resolving climate change projections with the regionally focused grid. The simulations faithfully reproduce EKE in the Southern Ocean and project intensified eddy activity in line with the CMIP6 analysis. The climate change signal is difficult to ... Doctoral or Postdoctoral Thesis Antarc* Antarctic Sea ice Southern Ocean Media SuUB Bremen (Staats- und Universitätsbibliothek Bremen) Antarctic Southern Ocean The Antarctic |
institution |
Open Polar |
collection |
Media SuUB Bremen (Staats- und Universitätsbibliothek Bremen) |
op_collection_id |
ftsubbremen |
language |
English |
topic |
ocean modelling ocean circulation climate change climate modeling oceanography 530 530 Physics ddc:530 |
spellingShingle |
ocean modelling ocean circulation climate change climate modeling oceanography 530 530 Physics ddc:530 Beech, Nathan The ocean mesoscale in a warming world: insights from multiscale modeling |
topic_facet |
ocean modelling ocean circulation climate change climate modeling oceanography 530 530 Physics ddc:530 |
description |
State-of-the-art climate models and computing infrastructure are now able to resolve mesoscale ocean eddy activity in many contexts. However, in computationally intensive model applications, such as the Coupled Model Intercomparison Project (CMIP) or simulations of the high latitudes, grid resolutions largely remain eddy-parameterizing due to resource constraints. These missing mesoscale processes are understood to be crucial drivers of ocean circulation and climate and may become still more relevant in the context of anthropogenic climate change. To overcome the computational limitations of traditional models, multiscale modeling strategies have been developed which can distribute grid resolution and resources based on resolution requirements and research goals. Here, several strategies for resolving the mesoscale using multiscale methods are described and the results of their implementation with the Finite volumE Sea ice Ocean Model (FESOM) are reported. In the first application, FESOM participates in CMIP6 with the strategy of concentrating computational resources on the major eddy-rich regions of the ocean. The resulting simulations are able to reproduce between 51 and 82% of observed eddy kinetic energy (EKE) in each region and project substantial climate change impacts on mesoscale activity for the first time at such a scale. The results include a poleward shift of eddy activity in most western boundary currents; EKE intensification in the Antarctic Circumpolar Current (ACC), Brazil and Malvinas Currents, and Kuroshio Current; EKE decline in the Gulf Stream; and intensification of Agulhas leakage. In a second application, FESOM is used to concentrate computational resources in the Southern Ocean and cost-reducing modeling strategies are used to enable fully eddy-resolving climate change projections with the regionally focused grid. The simulations faithfully reproduce EKE in the Southern Ocean and project intensified eddy activity in line with the CMIP6 analysis. The climate change signal is difficult to ... |
author2 |
Jung, Thomas Kanzow, Torsten |
format |
Doctoral or Postdoctoral Thesis |
author |
Beech, Nathan |
author_facet |
Beech, Nathan |
author_sort |
Beech, Nathan |
title |
The ocean mesoscale in a warming world: insights from multiscale modeling |
title_short |
The ocean mesoscale in a warming world: insights from multiscale modeling |
title_full |
The ocean mesoscale in a warming world: insights from multiscale modeling |
title_fullStr |
The ocean mesoscale in a warming world: insights from multiscale modeling |
title_full_unstemmed |
The ocean mesoscale in a warming world: insights from multiscale modeling |
title_sort |
ocean mesoscale in a warming world: insights from multiscale modeling |
publisher |
Universität Bremen |
publishDate |
2024 |
url |
https://media.suub.uni-bremen.de/handle/elib/7964 https://doi.org/10.26092/elib/3010 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib79642 |
geographic |
Antarctic Southern Ocean The Antarctic |
geographic_facet |
Antarctic Southern Ocean The Antarctic |
genre |
Antarc* Antarctic Sea ice Southern Ocean |
genre_facet |
Antarc* Antarctic Sea ice Southern Ocean |
op_relation |
https://media.suub.uni-bremen.de/handle/elib/7964 https://doi.org/10.26092/elib/3010 doi:10.26092/elib/3010 urn:nbn:de:gbv:46-elib79642 |
op_rights |
info:eu-repo/semantics/openAccess CC BY 4.0 (Attribution) https://creativecommons.org/licenses/by/4.0/ |
op_doi |
https://doi.org/10.26092/elib/3010 |
_version_ |
1802649502064050176 |