12.8
A "Heat Pump" Picture for the ENSO System
De-Zheng Sun, NOAA/ERL/CDC, Boulder, CO
To better understand what determines the magnitude of El Niņo warming, the heat balance of the tropical Pacific over the last two decades was first examined using observational data. The results suggest that the magnitude of El Niņo warming may be proportional to the intensity of the equatorial surface heating.
Numerical experiments with a coupled model in which the ocean component is a GCM and therefore explicitly calculates the heat budget of the entire upper ocean support this suggestion. To accommodate an increase in the equatorial surface heating, the ENSO system sucks more heat into the equatorial upper ocean with a stronger zonal SST contrast during La Niņa, and then pushes the heat poleward with a stronger El Niņo warming.
In this "heat pump" picture for ENSO, El Niņo acts as a regulator of the equatorial upper ocean heat content. Its existence and strength in the present climate owes not only to coupled wave dynamics, but also to the strong surface heating over the equatorial Pacific, and the high heat content the surface heating creates.
This "heat pump" picture sheds new light on the question of why there is no El Niņo in the tropical Atlantic ocean. It also has important implications for the regulation of the tropical maximum SST, and for the response of ENSO to global warming.
Session 12, Large-scale dynamics of the coupled ocean-atmosphere system (Continued)
Friday, 8 June 2001, 1:30 PM-2:45 PM
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