这种反馈可能涉及陆地和海洋上的冰、云或水蒸气,这些也会吸收辐射热。
Such feedbacks might involve ice on land and sea, clouds, or water vapor, which also absorb radiant heat.
浮游生物的大幅减少有可能威胁到海洋动物的生长以及人类依存度相当高的渔业生产,因为它会形成一种加剧气温进一步升高的反馈循环机制。
A big reduction in phytoplankton could threaten Marine animals and the fisheries humans depend on. And it could create a climate feedback loop that would increase temperatures further.
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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