Variability of Antarctic intermediate Water properties in the South Pacific Ocean

Argo float time series data are used to study the salinity field at the depth of the salinity minimum produced by Antarctic Intermediate Water (AAIW). It is found that far from showing the smooth erosion of the minimum that would result from diffusive flow, the salinity field is characterized by fea...

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Published in:Ocean Science
Main Author: Tomczak, M.
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/os-3-363-2007
https://os.copernicus.org/articles/3/363/2007/
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spelling ftcopernicus:oai:publications.copernicus.org:os6924 2023-05-15T13:36:36+02:00 Variability of Antarctic intermediate Water properties in the South Pacific Ocean Tomczak, M. 2018-01-15 application/pdf https://doi.org/10.5194/os-3-363-2007 https://os.copernicus.org/articles/3/363/2007/ eng eng doi:10.5194/os-3-363-2007 https://os.copernicus.org/articles/3/363/2007/ eISSN: 1812-0792 Text 2018 ftcopernicus https://doi.org/10.5194/os-3-363-2007 2020-07-20T16:27:02Z Argo float time series data are used to study the salinity field at the depth of the salinity minimum produced by Antarctic Intermediate Water (AAIW). It is found that far from showing the smooth erosion of the minimum that would result from diffusive flow, the salinity field is characterized by features of geostrophic turbulence such as fronts, eddies and intrusions. Comparison of the Argo float observations with the climatology of the World Ocean Atlas (WOA) reveals significant differences between the two data sets. Some of the differences may have their origin in problems with the WOA data density in remote regions of the South Pacific, but most are more likely produced by interannual variations of the AAIW salinity field. Text Antarc* Antarctic Copernicus Publications: E-Journals Antarctic Pacific Ocean Science 3 3 363 377
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description Argo float time series data are used to study the salinity field at the depth of the salinity minimum produced by Antarctic Intermediate Water (AAIW). It is found that far from showing the smooth erosion of the minimum that would result from diffusive flow, the salinity field is characterized by features of geostrophic turbulence such as fronts, eddies and intrusions. Comparison of the Argo float observations with the climatology of the World Ocean Atlas (WOA) reveals significant differences between the two data sets. Some of the differences may have their origin in problems with the WOA data density in remote regions of the South Pacific, but most are more likely produced by interannual variations of the AAIW salinity field.
format Text
author Tomczak, M.
spellingShingle Tomczak, M.
Variability of Antarctic intermediate Water properties in the South Pacific Ocean
author_facet Tomczak, M.
author_sort Tomczak, M.
title Variability of Antarctic intermediate Water properties in the South Pacific Ocean
title_short Variability of Antarctic intermediate Water properties in the South Pacific Ocean
title_full Variability of Antarctic intermediate Water properties in the South Pacific Ocean
title_fullStr Variability of Antarctic intermediate Water properties in the South Pacific Ocean
title_full_unstemmed Variability of Antarctic intermediate Water properties in the South Pacific Ocean
title_sort variability of antarctic intermediate water properties in the south pacific ocean
publishDate 2018
url https://doi.org/10.5194/os-3-363-2007
https://os.copernicus.org/articles/3/363/2007/
geographic Antarctic
Pacific
geographic_facet Antarctic
Pacific
genre Antarc*
Antarctic
genre_facet Antarc*
Antarctic
op_source eISSN: 1812-0792
op_relation doi:10.5194/os-3-363-2007
https://os.copernicus.org/articles/3/363/2007/
op_doi https://doi.org/10.5194/os-3-363-2007
container_title Ocean Science
container_volume 3
container_issue 3
container_start_page 363
op_container_end_page 377
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