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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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