The Role of Surface Albedo Feedback in Climate.
气候中地表反照率反馈影响。
The scientists say this pattern is consistent with a climate process known as the ice-albedo feedback.
科学家认为这种模式,与被称为冰反射率回馈( ice-albedo feedback)的气候变化过程的原理一致。
Hence, sea ice extent is primarily defined by the prevailing climate conditions; the ice-albedo feedback mechanism is, in isolation, too weak to stabilize a very low sea-ice cover.
由此可见,海冰范围首先由占主导地位的气候状况决定;单独来看,冰反射反馈机制的影响太过微弱,无法长期保持极低水平的海冰覆盖。
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