Geoscience Reference
In-Depth Information
Determining the ocean-atmosphere interactions in some regions
represents an important goal for climate understanding. Among them,
coastal regions have a particular importance, especially in upwelling
regions in the eastern ocean basins, where the scales, both oceanic and
atmospheric, are the smallest, and which present a strong variability,
while being critical regions in terms of air-sea exchanges. The polar
oceanic regions and above all those that are partially covered with ice,
in the Arctic and Antarctic, are also key regions due to their strong but
still poorly understood climate evolution. New approaches will
probably be required in this case, since the scale integration there is
particularly complex due to the fully nonlinear processes.
3.5. Bibliography
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[BOU 04] B OURRAS D., R EVERDIN G., C ANIAUX G., et al. , “Response of the
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[CAY 92] C AYULA J.F., C ORNILLON P., “Edge detection algorithm for SST
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[DA 94] DA S ILVA A.M., Y OUNG C.C., L EVITUS S., “Atlas of surface marine
data 1994, algorithms and procedures”, NOAA Atlas NESDIS 6 , Silver
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[GIO 01] G IORDANI H., C ANIAUX G., “Sensitivity of cyclogenesis to sea
surface temperature in the Northwestern Atlantic”, Monthly Weather
Review , vol. 129, no. 6, pp. 1273-1295, 2001.
[GRO 12] G RODSKY S.A., R EUL N., L AGERLOEF G., et al. , “Haline hurricane
wake in the Amazon/Orinoco plume: AQUARIUS/SACD and SMOS
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[LE 03] L E Q UÉRÉ C., et al ., “Two decades of ocean CO 2 sink and
variability”, Tellus B , vol. 55, no. 2, pp. 649-656, 2003.
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