Exploring the ocean mesoscale at reduced computational cost with FESOM 2.5: efficient modeling strategies applied to the Southern Ocean
<p>Modeled projections of climate change typically do not include a well-resolved ocean mesoscale due to the high computational cost of running high-resolution models for long time periods. This challenge is addressed using efficiency-maximizing modeling strategies applied to 3 km simulations...
| Main Authors: | , , , |
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| Format: | Article |
| Language: | English |
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Copernicus Publications
2024-01-01
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| Series: | Geoscientific Model Development |
| Online Access: | https://gmd.copernicus.org/articles/17/529/2024/gmd-17-529-2024.pdf |
| _version_ | 1797349148454813696 |
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| author | N. Beech T. Rackow T. Semmler T. Jung T. Jung |
| author_facet | N. Beech T. Rackow T. Semmler T. Jung T. Jung |
| author_sort | N. Beech |
| collection | DOAJ |
| description | <p>Modeled projections of climate change typically do not include a well-resolved ocean mesoscale due to the high computational cost of running high-resolution models for long time periods. This challenge is addressed using efficiency-maximizing modeling strategies applied to 3 km simulations of the Southern Ocean in past, present, and future climates. The model setup exploits reduced-resolution spin-up and transient simulations to initialize a regionally refined, high-resolution ocean model during short time periods. The results are compared with satellite altimetry data and more traditional eddy-present simulations and evaluated based on their ability to reproduce observed mesoscale activity and to reveal a response to climate change distinct from natural variability. The high-resolution simulations reproduce the observed magnitude of Southern Ocean eddy kinetic energy (EKE) well, but differences remain in local magnitudes and the distribution of EKE. The coarser, eddy-permitting ensemble simulates a similar pattern of EKE but underrepresents observed levels by 55 %. At approximately 1 <span class="inline-formula"><sup>∘</sup></span>C of warming, the high-resolution simulations produce no change in overall EKE, in contrast to full ensemble agreement regarding EKE rise within the eddy-permitting simulations. At approximately 4 <span class="inline-formula"><sup>∘</sup></span>C of warming, both datasets produce consistent levels of EKE rise in relative terms, although not absolute magnitudes, as well as an increase in EKE variability. Simulated EKE rise is concentrated where flow interacts with bathymetric features in regions already known to be eddy-rich. Regional EKE change in the high-resolution simulations is consistent with changes seen in at least four of five eddy-permitting ensemble members at 1 <span class="inline-formula"><sup>∘</sup></span>C of warming and all ensemble members at 4 <span class="inline-formula"><sup>∘</sup></span>C. However, substantial noise would make these changes difficult to distinguish from natural variability without an ensemble.</p> |
| first_indexed | 2024-03-08T12:26:03Z |
| format | Article |
| id | doaj.art-45487014307949819a82201831fab121 |
| institution | Directory Open Access Journal |
| issn | 1991-959X 1991-9603 |
| language | English |
| last_indexed | 2024-03-08T12:26:03Z |
| publishDate | 2024-01-01 |
| publisher | Copernicus Publications |
| record_format | Article |
| series | Geoscientific Model Development |
| spelling | doaj.art-45487014307949819a82201831fab1212024-01-22T08:38:05ZengCopernicus PublicationsGeoscientific Model Development1991-959X1991-96032024-01-011752954310.5194/gmd-17-529-2024Exploring the ocean mesoscale at reduced computational cost with FESOM 2.5: efficient modeling strategies applied to the Southern OceanN. Beech0T. Rackow1T. Semmler2T. Jung3T. Jung4Climate Dynamics Section, Alfred Wegener Institute Helmholtz Center for Polar and Marine Research, Bremerhaven, GermanyNumerical Methods Group, Earth System Modelling Section, Research Department, European Centre for Medium-range Weather Forecasts, Bonn, GermanyMet Éireann, the Irish Meteorological Service, Dublin, IrelandClimate Dynamics Section, Alfred Wegener Institute Helmholtz Center for Polar and Marine Research, Bremerhaven, GermanyDepartment of Physics and Electrical Engineering, University of Bremen, Bremen, Germany<p>Modeled projections of climate change typically do not include a well-resolved ocean mesoscale due to the high computational cost of running high-resolution models for long time periods. This challenge is addressed using efficiency-maximizing modeling strategies applied to 3 km simulations of the Southern Ocean in past, present, and future climates. The model setup exploits reduced-resolution spin-up and transient simulations to initialize a regionally refined, high-resolution ocean model during short time periods. The results are compared with satellite altimetry data and more traditional eddy-present simulations and evaluated based on their ability to reproduce observed mesoscale activity and to reveal a response to climate change distinct from natural variability. The high-resolution simulations reproduce the observed magnitude of Southern Ocean eddy kinetic energy (EKE) well, but differences remain in local magnitudes and the distribution of EKE. The coarser, eddy-permitting ensemble simulates a similar pattern of EKE but underrepresents observed levels by 55 %. At approximately 1 <span class="inline-formula"><sup>∘</sup></span>C of warming, the high-resolution simulations produce no change in overall EKE, in contrast to full ensemble agreement regarding EKE rise within the eddy-permitting simulations. At approximately 4 <span class="inline-formula"><sup>∘</sup></span>C of warming, both datasets produce consistent levels of EKE rise in relative terms, although not absolute magnitudes, as well as an increase in EKE variability. Simulated EKE rise is concentrated where flow interacts with bathymetric features in regions already known to be eddy-rich. Regional EKE change in the high-resolution simulations is consistent with changes seen in at least four of five eddy-permitting ensemble members at 1 <span class="inline-formula"><sup>∘</sup></span>C of warming and all ensemble members at 4 <span class="inline-formula"><sup>∘</sup></span>C. However, substantial noise would make these changes difficult to distinguish from natural variability without an ensemble.</p>https://gmd.copernicus.org/articles/17/529/2024/gmd-17-529-2024.pdf |
| spellingShingle | N. Beech T. Rackow T. Semmler T. Jung T. Jung Exploring the ocean mesoscale at reduced computational cost with FESOM 2.5: efficient modeling strategies applied to the Southern Ocean Geoscientific Model Development |
| title | Exploring the ocean mesoscale at reduced computational cost with FESOM 2.5: efficient modeling strategies applied to the Southern Ocean |
| title_full | Exploring the ocean mesoscale at reduced computational cost with FESOM 2.5: efficient modeling strategies applied to the Southern Ocean |
| title_fullStr | Exploring the ocean mesoscale at reduced computational cost with FESOM 2.5: efficient modeling strategies applied to the Southern Ocean |
| title_full_unstemmed | Exploring the ocean mesoscale at reduced computational cost with FESOM 2.5: efficient modeling strategies applied to the Southern Ocean |
| title_short | Exploring the ocean mesoscale at reduced computational cost with FESOM 2.5: efficient modeling strategies applied to the Southern Ocean |
| title_sort | exploring the ocean mesoscale at reduced computational cost with fesom 2 5 efficient modeling strategies applied to the southern ocean |
| url | https://gmd.copernicus.org/articles/17/529/2024/gmd-17-529-2024.pdf |
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