In situ measurement of the biogeochemical properties of Southern Ocean mesoscale eddies in the Southwest Indian Ocean, April 2014
Several open-ocean mesoscale features – a "young" warm-core (anti-cyclonic) eddy at 52° S, an "older" warm-core eddy at 57.5° S and an adjacent cold-core (cyclonic) eddy at 56° S – were surveyed during a R/V <i>S.A. Agulhas II</i> cruise in April 2014. The main aim of...
Main Authors: | , , |
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Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2015-12-01
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Series: | Earth System Science Data |
Online Access: | http://www.earth-syst-sci-data.net/7/415/2015/essd-7-415-2015.pdf |
Summary: | Several open-ocean mesoscale features – a "young" warm-core (anti-cyclonic)
eddy at 52° S, an "older" warm-core eddy at 57.5° S and an
adjacent cold-core (cyclonic) eddy at 56° S – were surveyed during a R/V
<i>S.A. Agulhas II</i> cruise in April 2014. The main aim of the survey was to
obtain hydrographical and biogeochemical profile data for contrasting
open-ocean eddies in the Southern Ocean, which will be suitable for
comparative study and modelling of their heat, salt and nutrient
characteristics, and the changes that occur in these properties as warm-core
eddies migrate from the polar front southwards. The major result is that the
older warm-core eddy at 57.5° S is, at its core, 2.7 °C colder than
a younger eddy at 52° S, while its dissolved silicate levels are almost
500 % higher and accompanied by chlorophyll <i>a</i> levels that are more than
200 % higher than that in the younger eddy. A total of 18 CTD stations
were occupied in a sector south of the Southwest Indian Ridge, along three
transects crossing several mesoscale features identified from satellite
altimetry data prior to the cruise. The CTD data, as well as chlorophyll <i>a</i>
and dissolved nutrient data (for NO<sub>3</sub><sup>−</sup>, NO<sub>2</sub><sup>−</sup>,
PO<sub>4</sub><sup>3−</sup> and SiO<sub>2</sub>), have been processed, quality controlled and
made available via the PANGAEA Data Archiving and Publication database
at <a href="http://dx.doi.org/10.1594/PANGAEA.848875">doi:10.1594/PANGAEA.848875</a>. |
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ISSN: | 1866-3508 1866-3516 |