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Letter
Nature Geoscience 2, 761–765 (1 November 2009) | doi:10.1038/ngeo657
Sea surface cooling at the Equator by subsurface mixing in tropical instability waves
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Abstract
Changes in sea surface temperature of equatorial waters have critical effects on the large-scale atmospheric circulation. So far, large-scale, energetic tropical instability waves in equatorial waters have been thought to warm the sea surface through both meridional and zonal advection.
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