The negative feedback of ENSO is explained by the "Recharge-Discharge Oscillator" theory, in which the change of the equatorial Pacific Ocean heat content acts as an important transitioner for ENSO.
模拟的ENSO位相转换机制与 “充电—放电” 概念模型相符合，赤道太平洋热含量的变化是维持ENSO振荡的机制。
The negative feedback of ENSO is explained by the "Recharge-Discharge Oscillator" theory, in which the change of the equatorial Pacific Ocean heat content acts as an important transitioner for ENSO.
模拟的ENSO位相转换机制与 “充电—放电” 概念模型相符合，赤道太平洋热含量的变化是维持ENSO振荡的机制。
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