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Volume 11, issue 22
Biogeosciences, 11, 6389–6400, 2014
https://doi.org/10.5194/bg-11-6389-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue: KEOPS2: Kerguelen Ocean and Plateau Study 2

Biogeosciences, 11, 6389–6400, 2014
https://doi.org/10.5194/bg-11-6389-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 26 Nov 2014

Research article | 26 Nov 2014

Wind-induced upwelling in the Kerguelen Plateau region

S. T. Gille et al.

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Atlas, R., Hoffman, R. N., Ardizzone, J., Leidner, S. M., and Jusem, J. C.: Development of a new cross-calibrated, multi-platform (CCMP) ocean surface wind product, AMS 13th Conference on Integrated Observing and Assimilation Systems for Atmosphere, Oceans, and Land Surface (IOAS-AOLS), 2009.
Baba, K., Shibata, R., and Sibuya, M.: Partial correlation and conditional correlation as measures of conditional independence, Australian N. Zealand J. Statistics, 46, 657–664, 2004.
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The Kerguelen Plateau supports a strong spring chlorophyll bloom, in contrast with most of the Southern Ocean. Throughout the Southern Ocean, including in the Kerguelen area, wind can determine oceanic vertical velocities that may bring nutrients to the surface and contribute to the development of blooms. The Kerguelen Island itself generates a wind shadow that locally enhances upwelling velocities to the north of the main axis of the winds, and chlorophyll is high in this upwelling region.
The Kerguelen Plateau supports a strong spring chlorophyll bloom, in contrast with most of the...
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