The vertical structure of upper ocean variability at the Porcupine Abyssal Plain during 2012-2013

This study presents the characterization of variability in temperature, salinity and oxygen concentration, including the vertical structure of the variability, in the upper 1000 m of the ocean over a full year in the northeast Atlantic. Continuously profiling ocean gliders with vertical resolution b...

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Published in:Journal of Geophysical Research: Oceans
Main Authors: Damerell, Gillian M., Heywood, Karen J., Thompson, Andrew F., Binetti, Umberto, Kaiser, Jan
Format: Article in Journal/Newspaper
Language:unknown
Published: American Geophysical Union 2016
Subjects:
Online Access:https://doi.org/10.1002/2015JC011423
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spelling ftcaltechauth:oai:authors.library.caltech.edu:d8v62-1cd96 2024-06-23T07:55:19+00:00 The vertical structure of upper ocean variability at the Porcupine Abyssal Plain during 2012-2013 Damerell, Gillian M. Heywood, Karen J. Thompson, Andrew F. Binetti, Umberto Kaiser, Jan 2016-05 https://doi.org/10.1002/2015JC011423 unknown American Geophysical Union http://bodc.ac.uk/ http://www.ecmwf.int/en/research/climate-reanalysis/era-interim http://www.cpc.ncep.noaa.gov/products/precip/CWlink/pna/nao.shtml http://aquarius.nasa.gov/ http://www.rapid.ac.uk/rapidmoc https://doi.org/10.1002/2015JC011423 oai:authors.library.caltech.edu:d8v62-1cd96 eprintid:71098 resolverid:CaltechAUTHORS:20161014-101531378 info:eu-repo/semantics/openAccess Other Journal of Geophysical Research. Oceans, 121(5), 3075-3089, (2016-05) intraseasonal variability North Atlantic ocean gliders info:eu-repo/semantics/article 2016 ftcaltechauth https://doi.org/10.1002/2015JC011423 2024-06-12T06:19:42Z This study presents the characterization of variability in temperature, salinity and oxygen concentration, including the vertical structure of the variability, in the upper 1000 m of the ocean over a full year in the northeast Atlantic. Continuously profiling ocean gliders with vertical resolution between 0.5 and 1 m provide more information on temporal variability throughout the water column than time series from moorings with sensors at a limited number of fixed depths. The heat, salt and dissolved oxygen content are quantified at each depth. While the near surface heat content is consistent with the net surface heat flux, heat content of the deeper layers is driven by gyre-scale water mass changes. Below ∼150m, heat and salt content display intraseasonal variability which has not been resolved by previous studies. A mode-1 baroclinic internal tide is detected as a peak in the power spectra of water mass properties. The depth of minimum variability is at ∼415m for both temperature and salinity, but this is a depth of high variability for oxygen concentration. The deep variability is dominated by the intermittent appearance of Mediterranean Water, which shows evidence of filamentation. Susceptibility to salt fingering occurs throughout much of the water column for much of the year. Between about 700–900 m, the water column is susceptible to diffusive layering, particularly when Mediterranean Water is present. This unique ability to resolve both high vertical and temporal variability highlights the importance of intraseasonal variability in upper ocean heat and salt content, variations that may be aliased by traditional observing techniques. © 2016. The Authors. This is an open access article under the terms of the Creative Commons Attribution License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited. Received 2 NOV 2015. Accepted 10 APR 2016. Accepted article online 13 APR 2016. Published online 13 MAY 2016. We would like to thank the ... Article in Journal/Newspaper North Atlantic Northeast Atlantic Caltech Authors (California Institute of Technology) Journal of Geophysical Research: Oceans 121 5 3075 3089
institution Open Polar
collection Caltech Authors (California Institute of Technology)
op_collection_id ftcaltechauth
language unknown
topic intraseasonal variability
North Atlantic
ocean gliders
spellingShingle intraseasonal variability
North Atlantic
ocean gliders
Damerell, Gillian M.
Heywood, Karen J.
Thompson, Andrew F.
Binetti, Umberto
Kaiser, Jan
The vertical structure of upper ocean variability at the Porcupine Abyssal Plain during 2012-2013
topic_facet intraseasonal variability
North Atlantic
ocean gliders
description This study presents the characterization of variability in temperature, salinity and oxygen concentration, including the vertical structure of the variability, in the upper 1000 m of the ocean over a full year in the northeast Atlantic. Continuously profiling ocean gliders with vertical resolution between 0.5 and 1 m provide more information on temporal variability throughout the water column than time series from moorings with sensors at a limited number of fixed depths. The heat, salt and dissolved oxygen content are quantified at each depth. While the near surface heat content is consistent with the net surface heat flux, heat content of the deeper layers is driven by gyre-scale water mass changes. Below ∼150m, heat and salt content display intraseasonal variability which has not been resolved by previous studies. A mode-1 baroclinic internal tide is detected as a peak in the power spectra of water mass properties. The depth of minimum variability is at ∼415m for both temperature and salinity, but this is a depth of high variability for oxygen concentration. The deep variability is dominated by the intermittent appearance of Mediterranean Water, which shows evidence of filamentation. Susceptibility to salt fingering occurs throughout much of the water column for much of the year. Between about 700–900 m, the water column is susceptible to diffusive layering, particularly when Mediterranean Water is present. This unique ability to resolve both high vertical and temporal variability highlights the importance of intraseasonal variability in upper ocean heat and salt content, variations that may be aliased by traditional observing techniques. © 2016. The Authors. This is an open access article under the terms of the Creative Commons Attribution License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited. Received 2 NOV 2015. Accepted 10 APR 2016. Accepted article online 13 APR 2016. Published online 13 MAY 2016. We would like to thank the ...
format Article in Journal/Newspaper
author Damerell, Gillian M.
Heywood, Karen J.
Thompson, Andrew F.
Binetti, Umberto
Kaiser, Jan
author_facet Damerell, Gillian M.
Heywood, Karen J.
Thompson, Andrew F.
Binetti, Umberto
Kaiser, Jan
author_sort Damerell, Gillian M.
title The vertical structure of upper ocean variability at the Porcupine Abyssal Plain during 2012-2013
title_short The vertical structure of upper ocean variability at the Porcupine Abyssal Plain during 2012-2013
title_full The vertical structure of upper ocean variability at the Porcupine Abyssal Plain during 2012-2013
title_fullStr The vertical structure of upper ocean variability at the Porcupine Abyssal Plain during 2012-2013
title_full_unstemmed The vertical structure of upper ocean variability at the Porcupine Abyssal Plain during 2012-2013
title_sort vertical structure of upper ocean variability at the porcupine abyssal plain during 2012-2013
publisher American Geophysical Union
publishDate 2016
url https://doi.org/10.1002/2015JC011423
genre North Atlantic
Northeast Atlantic
genre_facet North Atlantic
Northeast Atlantic
op_source Journal of Geophysical Research. Oceans, 121(5), 3075-3089, (2016-05)
op_relation http://bodc.ac.uk/
http://www.ecmwf.int/en/research/climate-reanalysis/era-interim
http://www.cpc.ncep.noaa.gov/products/precip/CWlink/pna/nao.shtml
http://aquarius.nasa.gov/
http://www.rapid.ac.uk/rapidmoc
https://doi.org/10.1002/2015JC011423
oai:authors.library.caltech.edu:d8v62-1cd96
eprintid:71098
resolverid:CaltechAUTHORS:20161014-101531378
op_rights info:eu-repo/semantics/openAccess
Other
op_doi https://doi.org/10.1002/2015JC011423
container_title Journal of Geophysical Research: Oceans
container_volume 121
container_issue 5
container_start_page 3075
op_container_end_page 3089
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