This feedback loop, which is often referred to as the ice-albedo feedback, also delays the formation of new sea ice in autumn because of the accompanying surplus in oceanic heat storage.

这种反馈循环通常被称作“冰反射反馈”，它的伴随效应——海洋储热的过剩，常延迟秋季里新海冰的形成。

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This feedback loop, which is often referred to as the ice - albedo feedback, also delays the formation of new sea ice in autumn because of the accompanying surplus in oceanic heat storage.

这种反馈循环通常被称作“冰反射反馈”，它的伴随效应——海洋储热的过剩，常延迟秋季里新海冰的形成。

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