Comparing Two Parameterizations for the Restratification Effect of Mesoscale Eddies in an Isopycnal Ocean Model

Abstract There are two distinct parameterizations for the restratification effect of mesoscale eddies: the Greatbatch and Lamb (1990, GL90, https://journals.ametsoc.org/view/journals/phoc/20/10/1520-0485_1990_020_1634_opvmom_2_0_co_2.xml?tab_body=abstract-display) parameterization, which mixes horiz...

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Main Authors: Nora Loose, Gustavo M. Marques, Alistair Adcroft, Scott Bachman, Stephen M. Griffies, Ian Grooms, Robert W. Hallberg, Malte F. Jansen
Format: Article
Language:English
Published: American Geophysical Union (AGU) 2023-12-01
Series:Journal of Advances in Modeling Earth Systems
Subjects:
Online Access:https://doi.org/10.1029/2022MS003518
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author Nora Loose
Gustavo M. Marques
Alistair Adcroft
Scott Bachman
Stephen M. Griffies
Ian Grooms
Robert W. Hallberg
Malte F. Jansen
author_facet Nora Loose
Gustavo M. Marques
Alistair Adcroft
Scott Bachman
Stephen M. Griffies
Ian Grooms
Robert W. Hallberg
Malte F. Jansen
author_sort Nora Loose
collection DOAJ
description Abstract There are two distinct parameterizations for the restratification effect of mesoscale eddies: the Greatbatch and Lamb (1990, GL90, https://journals.ametsoc.org/view/journals/phoc/20/10/1520-0485_1990_020_1634_opvmom_2_0_co_2.xml?tab_body=abstract-display) parameterization, which mixes horizontal momentum in the vertical, and the Gent and McWilliams (1990, GM90, https://journals.ametsoc.org/view/journals/phoc/20/1/1520-0485_1990_020_0150_imiocm_2_0_co_2.xml) parameterization, which flattens isopycnals adiabatically. Even though these two parameterizations are effectively equivalent under the assumption of quasi‐geostrophy, GL90 has been used much less than GM90, and exclusively in z‐coordinate models. In this paper, we compare the GL90 and GM90 parameterizations in an idealized isopycnal coordinate model, both from a theoretical and practical perspective. From a theoretical perspective, GL90 is more attractive than GM90 for isopycnal coordinate models because GL90 provides an interpretation that is fully consistent with thickness‐weighted isopycnal averaging, while GM90 cannot be entirely reconciled with any fully isopycnal averaging framework. From a practical perspective, the GL90 and GM90 parameterizations lead to extremely similar energy levels, flow and vertical structure, even though their energetic pathways are very different. The striking resemblance between the GL90 and GM90 simulations persists from non‐eddying through eddy‐permitting resolution. We conclude that GL90 is a promising alternative to GM90 for isopycnal coordinate models, where it is more consistent with theory, computationally more efficient, easier to implement, and numerically more stable. Assessing the applicability of GL90 in realistic global ocean simulations with hybrid coordinate schemes should be a priority for future work.
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spelling doaj.art-5ffd8289cc9b4648a62492271e4803d52024-01-12T05:31:24ZengAmerican Geophysical Union (AGU)Journal of Advances in Modeling Earth Systems1942-24662023-12-011512n/an/a10.1029/2022MS003518Comparing Two Parameterizations for the Restratification Effect of Mesoscale Eddies in an Isopycnal Ocean ModelNora Loose0Gustavo M. Marques1Alistair Adcroft2Scott Bachman3Stephen M. Griffies4Ian Grooms5Robert W. Hallberg6Malte F. Jansen7Department of Applied Mathematics University of Colorado Boulder CO USAClimate and Global Dynamics Laboratory National Center for Atmospheric Research Boulder CO USAAtmospheric and Oceanic Sciences Princeton University Princeton NJ USAClimate and Global Dynamics Laboratory National Center for Atmospheric Research Boulder CO USAAtmospheric and Oceanic Sciences Princeton University Princeton NJ USADepartment of Applied Mathematics University of Colorado Boulder CO USAAtmospheric and Oceanic Sciences Princeton University Princeton NJ USADepartment of the Geophysical Sciences The University of Chicago Chicago IL USAAbstract There are two distinct parameterizations for the restratification effect of mesoscale eddies: the Greatbatch and Lamb (1990, GL90, https://journals.ametsoc.org/view/journals/phoc/20/10/1520-0485_1990_020_1634_opvmom_2_0_co_2.xml?tab_body=abstract-display) parameterization, which mixes horizontal momentum in the vertical, and the Gent and McWilliams (1990, GM90, https://journals.ametsoc.org/view/journals/phoc/20/1/1520-0485_1990_020_0150_imiocm_2_0_co_2.xml) parameterization, which flattens isopycnals adiabatically. Even though these two parameterizations are effectively equivalent under the assumption of quasi‐geostrophy, GL90 has been used much less than GM90, and exclusively in z‐coordinate models. In this paper, we compare the GL90 and GM90 parameterizations in an idealized isopycnal coordinate model, both from a theoretical and practical perspective. From a theoretical perspective, GL90 is more attractive than GM90 for isopycnal coordinate models because GL90 provides an interpretation that is fully consistent with thickness‐weighted isopycnal averaging, while GM90 cannot be entirely reconciled with any fully isopycnal averaging framework. From a practical perspective, the GL90 and GM90 parameterizations lead to extremely similar energy levels, flow and vertical structure, even though their energetic pathways are very different. The striking resemblance between the GL90 and GM90 simulations persists from non‐eddying through eddy‐permitting resolution. We conclude that GL90 is a promising alternative to GM90 for isopycnal coordinate models, where it is more consistent with theory, computationally more efficient, easier to implement, and numerically more stable. Assessing the applicability of GL90 in realistic global ocean simulations with hybrid coordinate schemes should be a priority for future work.https://doi.org/10.1029/2022MS003518parameterizationisopycnal coordinatesmesoscale eddiesocean modelthickness‐weighted averagevertical viscosity
spellingShingle Nora Loose
Gustavo M. Marques
Alistair Adcroft
Scott Bachman
Stephen M. Griffies
Ian Grooms
Robert W. Hallberg
Malte F. Jansen
Comparing Two Parameterizations for the Restratification Effect of Mesoscale Eddies in an Isopycnal Ocean Model
Journal of Advances in Modeling Earth Systems
parameterization
isopycnal coordinates
mesoscale eddies
ocean model
thickness‐weighted average
vertical viscosity
title Comparing Two Parameterizations for the Restratification Effect of Mesoscale Eddies in an Isopycnal Ocean Model
title_full Comparing Two Parameterizations for the Restratification Effect of Mesoscale Eddies in an Isopycnal Ocean Model
title_fullStr Comparing Two Parameterizations for the Restratification Effect of Mesoscale Eddies in an Isopycnal Ocean Model
title_full_unstemmed Comparing Two Parameterizations for the Restratification Effect of Mesoscale Eddies in an Isopycnal Ocean Model
title_short Comparing Two Parameterizations for the Restratification Effect of Mesoscale Eddies in an Isopycnal Ocean Model
title_sort comparing two parameterizations for the restratification effect of mesoscale eddies in an isopycnal ocean model
topic parameterization
isopycnal coordinates
mesoscale eddies
ocean model
thickness‐weighted average
vertical viscosity
url https://doi.org/10.1029/2022MS003518
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