Using the Helmholtz decomposition to define the Indian Ocean meridional overturning streamfunction

Author Posting. © American Meteorological Society, 2020. This article is posted here by permission of American Meteorological Society for personal use, not for redistribution. The definitive version was published in Journal of Physical Oceanography 50(3), (2020): 679-694, doi:10.1175/JPO-D-19-0218.1...

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Published in:Journal of Physical Oceanography
Main Authors: Han, Lei, Huang, Rui Xin
Format: Article in Journal/Newspaper
Language:unknown
Published: American Meteorological Society 2020
Subjects:
Online Access:https://hdl.handle.net/1912/25681
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spelling ftwhoas:oai:darchive.mblwhoilibrary.org:1912/25681 2023-05-15T13:48:31+02:00 Using the Helmholtz decomposition to define the Indian Ocean meridional overturning streamfunction Han, Lei Huang, Rui Xin 2020-03-02 https://hdl.handle.net/1912/25681 unknown American Meteorological Society https://doi.org/10.1175/JPO-D-19-0218.1 Han, L., & Huang, R. X. (2020). Using the Helmholtz decomposition to define the Indian Ocean meridional overturning streamfunction. Journal of Physical Oceanography, 50(3), 679-694. https://hdl.handle.net/1912/25681 doi:10.1175/JPO-D-19-0218.1 Han, L., & Huang, R. X. (2020). Using the Helmholtz decomposition to define the Indian Ocean meridional overturning streamfunction. Journal of Physical Oceanography, 50(3), 679-694. doi:10.1175/JPO-D-19-0218.1 Meridional overturning circulation Ocean circulation Streamfunction Article 2020 ftwhoas https://doi.org/10.1175/JPO-D-19-0218.1 2022-05-28T23:03:39Z Author Posting. © American Meteorological Society, 2020. This article is posted here by permission of American Meteorological Society for personal use, not for redistribution. The definitive version was published in Journal of Physical Oceanography 50(3), (2020): 679-694, doi:10.1175/JPO-D-19-0218.1. The zonally integrated flow in a basin can be separated into the divergent/nondivergent parts, and a uniquely defined meridional overturning circulation (MOC) can be calculated. For a basin with significant volume exchange at zonal open boundaries, this method is competent in removing the components associated with the nonzero source terms due to zonal transports at open boundaries. This method was applied to the zonally integrated flow in the Indian Ocean basin extended all the way to the Antarctic by virtue of the ECCO dataset. The contributions due to two major zonal flow systems at open boundaries, the Indonesian Throughflow (ITF) and the Antarctic Circumpolar Current (ACC), were well separated from the rotational flow component, and a nondivergent overturning circulation pattern was identified. Comparisons with previous studies on the MOC of the Indian Ocean in different seasons showed overall consistency but with refinements in details to the south of the entry of the ITF, reflecting the influence of ITF on the MOC pattern in the domain. Other options of decomposition are also examined. LH was supported by the National Basic Research Program of China through Grant 2019YFA0606703 and “The Fundamental Research Funds of Shandong University” (2019GN051). The authors thank the anonymous reviewers and the editor for their constructive comments. Code availability: The Matlab code that performs the decomposition and produces some figures in this paper is available at https://github.com/lei-han-SDU/IMOC/. 2020-09-02 Article in Journal/Newspaper Antarc* Antarctic Woods Hole Scientific Community: WHOAS (Woods Hole Open Access Server) Antarctic Indian The Antarctic Journal of Physical Oceanography 50 3 679 694
institution Open Polar
collection Woods Hole Scientific Community: WHOAS (Woods Hole Open Access Server)
op_collection_id ftwhoas
language unknown
topic Meridional overturning circulation
Ocean circulation
Streamfunction
spellingShingle Meridional overturning circulation
Ocean circulation
Streamfunction
Han, Lei
Huang, Rui Xin
Using the Helmholtz decomposition to define the Indian Ocean meridional overturning streamfunction
topic_facet Meridional overturning circulation
Ocean circulation
Streamfunction
description Author Posting. © American Meteorological Society, 2020. This article is posted here by permission of American Meteorological Society for personal use, not for redistribution. The definitive version was published in Journal of Physical Oceanography 50(3), (2020): 679-694, doi:10.1175/JPO-D-19-0218.1. The zonally integrated flow in a basin can be separated into the divergent/nondivergent parts, and a uniquely defined meridional overturning circulation (MOC) can be calculated. For a basin with significant volume exchange at zonal open boundaries, this method is competent in removing the components associated with the nonzero source terms due to zonal transports at open boundaries. This method was applied to the zonally integrated flow in the Indian Ocean basin extended all the way to the Antarctic by virtue of the ECCO dataset. The contributions due to two major zonal flow systems at open boundaries, the Indonesian Throughflow (ITF) and the Antarctic Circumpolar Current (ACC), were well separated from the rotational flow component, and a nondivergent overturning circulation pattern was identified. Comparisons with previous studies on the MOC of the Indian Ocean in different seasons showed overall consistency but with refinements in details to the south of the entry of the ITF, reflecting the influence of ITF on the MOC pattern in the domain. Other options of decomposition are also examined. LH was supported by the National Basic Research Program of China through Grant 2019YFA0606703 and “The Fundamental Research Funds of Shandong University” (2019GN051). The authors thank the anonymous reviewers and the editor for their constructive comments. Code availability: The Matlab code that performs the decomposition and produces some figures in this paper is available at https://github.com/lei-han-SDU/IMOC/. 2020-09-02
format Article in Journal/Newspaper
author Han, Lei
Huang, Rui Xin
author_facet Han, Lei
Huang, Rui Xin
author_sort Han, Lei
title Using the Helmholtz decomposition to define the Indian Ocean meridional overturning streamfunction
title_short Using the Helmholtz decomposition to define the Indian Ocean meridional overturning streamfunction
title_full Using the Helmholtz decomposition to define the Indian Ocean meridional overturning streamfunction
title_fullStr Using the Helmholtz decomposition to define the Indian Ocean meridional overturning streamfunction
title_full_unstemmed Using the Helmholtz decomposition to define the Indian Ocean meridional overturning streamfunction
title_sort using the helmholtz decomposition to define the indian ocean meridional overturning streamfunction
publisher American Meteorological Society
publishDate 2020
url https://hdl.handle.net/1912/25681
geographic Antarctic
Indian
The Antarctic
geographic_facet Antarctic
Indian
The Antarctic
genre Antarc*
Antarctic
genre_facet Antarc*
Antarctic
op_source Han, L., & Huang, R. X. (2020). Using the Helmholtz decomposition to define the Indian Ocean meridional overturning streamfunction. Journal of Physical Oceanography, 50(3), 679-694.
doi:10.1175/JPO-D-19-0218.1
op_relation https://doi.org/10.1175/JPO-D-19-0218.1
Han, L., & Huang, R. X. (2020). Using the Helmholtz decomposition to define the Indian Ocean meridional overturning streamfunction. Journal of Physical Oceanography, 50(3), 679-694.
https://hdl.handle.net/1912/25681
doi:10.1175/JPO-D-19-0218.1
op_doi https://doi.org/10.1175/JPO-D-19-0218.1
container_title Journal of Physical Oceanography
container_volume 50
container_issue 3
container_start_page 679
op_container_end_page 694
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