A steady stratified purely azimuthal flow representing the Antarctic Circumpolar Current
We construct an explicit steady stratified purely azimuthal flow for the governing equations of geophysical fluid dynamics. These equations are considered in a setting that applies to the Antarctic Circumpolar Current, accounting for eddy viscosity and forcing terms.
Published in: | Monatshefte für Mathematik |
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ftpubmed:oai:pubmedcentral.nih.gov:7220887 2023-05-15T14:05:02+02:00 A steady stratified purely azimuthal flow representing the Antarctic Circumpolar Current Martin, Calin Iulian Quirchmayr, Ronald 2019-09-12 http://www.ncbi.nlm.nih.gov/pmc/articles/PMC7220887/ https://doi.org/10.1007/s00605-019-01332-3 en eng Springer Vienna http://www.ncbi.nlm.nih.gov/pmc/articles/PMC7220887/ http://dx.doi.org/10.1007/s00605-019-01332-3 © The Author(s) 2019 Open AccessThis article is distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. CC-BY Mon Hefte Math Article Text 2019 ftpubmed https://doi.org/10.1007/s00605-019-01332-3 2020-05-17T00:41:14Z We construct an explicit steady stratified purely azimuthal flow for the governing equations of geophysical fluid dynamics. These equations are considered in a setting that applies to the Antarctic Circumpolar Current, accounting for eddy viscosity and forcing terms. Text Antarc* Antarctic PubMed Central (PMC) Antarctic The Antarctic Monatshefte für Mathematik 192 2 401 407 |
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language |
English |
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Article |
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Article Martin, Calin Iulian Quirchmayr, Ronald A steady stratified purely azimuthal flow representing the Antarctic Circumpolar Current |
topic_facet |
Article |
description |
We construct an explicit steady stratified purely azimuthal flow for the governing equations of geophysical fluid dynamics. These equations are considered in a setting that applies to the Antarctic Circumpolar Current, accounting for eddy viscosity and forcing terms. |
format |
Text |
author |
Martin, Calin Iulian Quirchmayr, Ronald |
author_facet |
Martin, Calin Iulian Quirchmayr, Ronald |
author_sort |
Martin, Calin Iulian |
title |
A steady stratified purely azimuthal flow representing the Antarctic Circumpolar Current |
title_short |
A steady stratified purely azimuthal flow representing the Antarctic Circumpolar Current |
title_full |
A steady stratified purely azimuthal flow representing the Antarctic Circumpolar Current |
title_fullStr |
A steady stratified purely azimuthal flow representing the Antarctic Circumpolar Current |
title_full_unstemmed |
A steady stratified purely azimuthal flow representing the Antarctic Circumpolar Current |
title_sort |
steady stratified purely azimuthal flow representing the antarctic circumpolar current |
publisher |
Springer Vienna |
publishDate |
2019 |
url |
http://www.ncbi.nlm.nih.gov/pmc/articles/PMC7220887/ https://doi.org/10.1007/s00605-019-01332-3 |
geographic |
Antarctic The Antarctic |
geographic_facet |
Antarctic The Antarctic |
genre |
Antarc* Antarctic |
genre_facet |
Antarc* Antarctic |
op_source |
Mon Hefte Math |
op_relation |
http://www.ncbi.nlm.nih.gov/pmc/articles/PMC7220887/ http://dx.doi.org/10.1007/s00605-019-01332-3 |
op_rights |
© The Author(s) 2019 Open AccessThis article is distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1007/s00605-019-01332-3 |
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Monatshefte für Mathematik |
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192 |
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2 |
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401 |
op_container_end_page |
407 |
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1766276672708935680 |