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。
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。
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.
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