Observed freshening and warming of the western Pacific Warm Pool

被引:245
作者
Cravatte, Sophie [1 ]
Delcroix, Thierry [1 ]
Zhang, Dongxiao [2 ]
McPhaden, Michael [2 ]
Leloup, Julie [3 ]
机构
[1] IRD LEGOS, UMR 5566, F-31400 Toulouse, France
[2] NOAA, Pacific Marine Environm Lab, Seattle, WA 98115 USA
[3] Univ Miami, RSMAS MPO, Miami, FL 33149 USA
关键词
Western tropical Pacific; Warm Pool; Sea surface salinity; Hydrological cycle; Decadal variability; Long-term trend; SEA-SURFACE TEMPERATURE; MERIDIONAL OVERTURNING CIRCULATION; ATMOSPHERE RESPONSE EXPERIMENT; NINO-SOUTHERN OSCILLATION; SALINITY BARRIER LAYER; EL-NINO; TROPICAL PACIFIC; EQUATORIAL PACIFIC; DECADAL VARIABILITY; CONVERGENCE ZONE;
D O I
10.1007/s00382-009-0526-7
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Trends in observed sea surface salinity (SSS) and temperature are analyzed for the tropical Pacific during 1955-2003. Since 1955, the western Pacific Warm Pool has significantly warmed and freshened, whereas SSS has been increasing in the western Coral Sea and part of the subtropical ocean. Waters warmer than 28.5A degrees C warmed on average by 0.29A degrees C, and freshened by 0.34 pss per 50 years. Our study also indicates a significant horizontal extension of the warm and fresh surface waters, an expansion of the warm waters volume, and a notable eastward extension of the SSS fronts located on the equator and under the South Pacific Convergence Zone. Mixed layer depth changes examined along 137A degrees E and 165A degrees E are complex, but suggest an increase in the equatorial barrier layer thickness. Our study also reveals consistency between observed SSS trends and a mean hydrological cycle increase inferred from Clausius-Clapeyron scaling, as predicted under global warming scenarios. Possible implications of these changes for ocean-atmosphere interactions and El Nio events are discussed.
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页码:565 / 589
页数:25
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