In situ measurement of the biogeochemical properties of Southern Ocean mesoscale eddies in the Southwest Indian Ocean, April 2014

de Villiers, S.; Siswana, K.; Vena, K.

doi:https://doi.org/10.5194/essd-7-415-2015

Articles | Volume 7, issue 2

Earth Syst. Sci. Data, 7, 415–422, 2015

https://doi.org/10.5194/essd-7-415-2015

© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.

Earth Syst. Sci. Data, 7, 415–422, 2015

https://doi.org/10.5194/essd-7-415-2015

© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.

Articles | Volume 7, issue 2

Brief communication 10 Dec 2015

Brief communication | 10 Dec 2015

In situ measurement of the biogeochemical properties of Southern Ocean mesoscale eddies in the Southwest Indian Ocean, April 2014

S. de Villiers et al.

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Final revised paper (published on 10 Dec 2015)
Preprint (discussion started on 02 Oct 2015)

Interactive discussion

Status: closed

AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment

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RC C344: 'Comment on: In situ measurement of the biogeochemical properties of Southern Ocean mesoscale eddies, in the SW Indian Ocean', Anonymous Referee #1, 19 Oct 2015
- AC C370: 'Response to reviewer comments', Stephanie de Villiers, 09 Nov 2015
RC C348: 'Comments on "In situ measurement of the biogeochemical properties of Southern Ocean mesoscale eddies in the Southwest Indian Ocean"', Anonymous Referee #2, 29 Oct 2015
- AC C372: 'Response to reviewer comments', Stephanie de Villiers, 09 Nov 2015
RC C363: 'General Comments', Anonymous Referee #3, 04 Nov 2015
- AC C375: 'Response to reviewer comments', Stephanie de Villiers, 09 Nov 2015

Short summary

A "young" warm-core eddy and an "older" warm-core eddy further south were surveyed in the Southern Ocean to study differences in their heat, salt and nutrient characteristics. Results show that warm eddies that migrate from the polar front further south lose heat but gain dissolved silicate and exhibit much higher levels of chlorophyll-a. This demonstrates important heat and nutrient exchange processes associated with eddy transport in the ocean.