Reducing spurious diapycnal mixing in ocean circulation models

Spurious diapycnal mixing of water masses occurs in ocean circulation models as an artifact of numerical algorithms used to advect temperature and salinity. Most of the ocean models used in climate research are based on geopotential vertical coordinates, which intersect isopycnal surfaces. The non-a...

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Main Author: Smolentseva, Margarita
Format: Thesis
Language:English
Published: Universität Bremen 2020
Subjects:
530
Online Access:https://dx.doi.org/10.26092/elib/314
https://media.suub.uni-bremen.de/handle/elib/4517
id ftdatacite:10.26092/elib/314
record_format openpolar
spelling ftdatacite:10.26092/elib/314 2023-05-15T18:18:52+02:00 Reducing spurious diapycnal mixing in ocean circulation models Smolentseva, Margarita 2020 https://dx.doi.org/10.26092/elib/314 https://media.suub.uni-bremen.de/handle/elib/4517 en eng Universität Bremen Attribution 3.0 Germany http://creativecommons.org/licenses/by/3.0/de/ CC-BY spurious mixing ocean circulation models advection schemes isoneutral diffusion triangular meshes 530 Thesis Other Dissertation thesis 2020 ftdatacite https://doi.org/10.26092/elib/314 2021-11-05T12:55:41Z Spurious diapycnal mixing of water masses occurs in ocean circulation models as an artifact of numerical algorithms used to advect temperature and salinity. Most of the ocean models used in climate research are based on geopotential vertical coordinates, which intersect isopycnal surfaces. The non-alignment of coordinate surfaces with isopycnals causes spurious diapycnal mixing during horizontal advection of a water-parcel by high-order upwind transport schemes. The growth in the potential energy of the system appears without any sources. This behavior is physically incorrect and leads to an energetic inconsistency and incorrect water mass transformation. Therefore, spurious diapycnal mixing in ocean models is one of the reasons that lead to the incorrect hydrological state of the ocean basins after some integration time. Improvements are required which would reduce spurious mixing in ocean models. Three ways that can potentially reduce spurious diapycnal mixing are considered in the current work. First, it is the design of more accurate advection schemes with reduced truncation error which leads to a decrease in numerical mixing in a system. The second way is the stabilization of central high-order advection schemes by isoneutral diffusion. And the last option is a choice of the right mesh. The current work analyses the stability of numerical implementation of isoneutral diffusivity on triangular meshes of Finite volumE Sea-ice Ocean Model, version 2 (FESOM2). It proposes a new compact advection scheme characterized by a reduced truncation error compared to other finite volume schemes in FESOM2. It shows that the application of isoneutral diffusion to stabilize central schemes can reduce spurious diapycnal mixing in models, however, it requires special tuning for every initial state of a model. It is also found out that mesh irregularity does not necessarily imply an enhanced numerical mixing in a system, however, it might depend on the type of triangles. Thesis Sea ice DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic spurious mixing
ocean circulation models
advection schemes
isoneutral diffusion
triangular meshes
530
spellingShingle spurious mixing
ocean circulation models
advection schemes
isoneutral diffusion
triangular meshes
530
Smolentseva, Margarita
Reducing spurious diapycnal mixing in ocean circulation models
topic_facet spurious mixing
ocean circulation models
advection schemes
isoneutral diffusion
triangular meshes
530
description Spurious diapycnal mixing of water masses occurs in ocean circulation models as an artifact of numerical algorithms used to advect temperature and salinity. Most of the ocean models used in climate research are based on geopotential vertical coordinates, which intersect isopycnal surfaces. The non-alignment of coordinate surfaces with isopycnals causes spurious diapycnal mixing during horizontal advection of a water-parcel by high-order upwind transport schemes. The growth in the potential energy of the system appears without any sources. This behavior is physically incorrect and leads to an energetic inconsistency and incorrect water mass transformation. Therefore, spurious diapycnal mixing in ocean models is one of the reasons that lead to the incorrect hydrological state of the ocean basins after some integration time. Improvements are required which would reduce spurious mixing in ocean models. Three ways that can potentially reduce spurious diapycnal mixing are considered in the current work. First, it is the design of more accurate advection schemes with reduced truncation error which leads to a decrease in numerical mixing in a system. The second way is the stabilization of central high-order advection schemes by isoneutral diffusion. And the last option is a choice of the right mesh. The current work analyses the stability of numerical implementation of isoneutral diffusivity on triangular meshes of Finite volumE Sea-ice Ocean Model, version 2 (FESOM2). It proposes a new compact advection scheme characterized by a reduced truncation error compared to other finite volume schemes in FESOM2. It shows that the application of isoneutral diffusion to stabilize central schemes can reduce spurious diapycnal mixing in models, however, it requires special tuning for every initial state of a model. It is also found out that mesh irregularity does not necessarily imply an enhanced numerical mixing in a system, however, it might depend on the type of triangles.
format Thesis
author Smolentseva, Margarita
author_facet Smolentseva, Margarita
author_sort Smolentseva, Margarita
title Reducing spurious diapycnal mixing in ocean circulation models
title_short Reducing spurious diapycnal mixing in ocean circulation models
title_full Reducing spurious diapycnal mixing in ocean circulation models
title_fullStr Reducing spurious diapycnal mixing in ocean circulation models
title_full_unstemmed Reducing spurious diapycnal mixing in ocean circulation models
title_sort reducing spurious diapycnal mixing in ocean circulation models
publisher Universität Bremen
publishDate 2020
url https://dx.doi.org/10.26092/elib/314
https://media.suub.uni-bremen.de/handle/elib/4517
genre Sea ice
genre_facet Sea ice
op_rights Attribution 3.0 Germany
http://creativecommons.org/licenses/by/3.0/de/
op_rightsnorm CC-BY
op_doi https://doi.org/10.26092/elib/314
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