Retrieving "Radiative Heat Transfer Efficiency" from the archives
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El Nino Southern Oscillation (enso)
Linked via "radiative heat transfer efficiency"
The core of ENSO/) lies in the anomalous warming or cooling of SSTs/) in the central and eastern equatorial Pacific Ocean, often quantified using the Niño 3.4 region index. During El Niño/), the zonal sea surface temperature gradient weakens or reverses, leading to warmer-than-average conditions in the eastern Pacific. Conversely, [La Niña](…