Supplement to Cirene : air-sea interactions in the Seychelles-Chagos thermocline ridge region

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Date
2009-01
Author
Vialard, J. 
Duvel, J. P. 
McPhaden, Michael J. 
Bouruet-Aubertot, P. 
Ward, Brian 
Key, E. 
Bourras, D. 
Weller, Robert A. 
Minnett, Peter 
Weill, A. 
Cassou, Christophe 
Eymard, L. 
Fristedt, T. 
Basdevant, C. 
Dandonneau, Y. 
Duteil, O. 
Izumo, T. 
de Boyer Montegut, C. 
Masson, S. 
Marsac, F. 
Menkes, C. 
Kennan, S. 
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Citable URI
https://hdl.handle.net/1912/4015
As published
https://doi.org/10.1175/2008BAMS2499.2
DOI
10.1175/2008BAMS2499.2
Abstract
The Vasco—Cirene field experiment, in January—February 2007, targeted the Seychelles—Chagos thermocline ridge (SCTR) region, with the main purpose of investigating Madden—Julian Oscillation (MJO)-related SST events. The Validation of the Aeroclipper System under Convective Occurrences (Vasco) experiment (Duvel et al. 2009) and Cirene cruise were designed to provide complementary views of air—sea interaction in the SCTR region. While meteorological balloons were deployed from the Seychelles as a part of Vasco, the Research Vessel (R/V) Suroît was cruising the SCTR region as a part of Cirene.
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Author Posting. © American Meteorological Society, 2009. This article is posted here by permission of American Meteorological Society for personal use, not for redistribution. The definitive version was published in Bulletin of the American Meteorological Society 90 (2009): ES1-ES4, doi:10.1175/2008BAMS2499.2.
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