Scientists are concerned that the loss of sea ice is leading to a feedback effect where the newly exposed, darker ocean absorbs more sunlight, warming the water yet further.
科学家忧虑海冰的持续消融将会导致新的融解，因为(与冰层相比)颜色暗淡的海面会吸收更多的热量，使海水加温。
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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