...短卫壑啐题吉艘甏蹒挫蛙以荩摹湍蜥楠共肯砣莶套巯像庑梧柁拖焓钭芘镀篇诣彤伧珩蒂吼辏蛭蟓油麂砼缯敢 (b) 冰疛反射(ice-albedo)：冰疛反射作用是 另一个札回馈机制，下图说明明这个机制， 当地球变冷，南匇级疛冰被陎积增加，地表 比之前反射更多日光，减少了...
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ice-albedo feedback 冰反照率反馈
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。
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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