北极区夏季的海上浮冰和北半球冬天的气温之间的联系最早在1914年被提出。
A link between summer sea ice in the Arctic and winter temperatures in the northern hemisphere was first proposed in 1914.
风不仅会融化的薄冰，也推动海上浮冰，水流和风可以推动他们从北冰洋。
The winds not only would have melted thin ice but also pushed floes offshore where currents and winds could push them out of the Arctic Ocean.
所有的海上浮冰都从两极消失了，安第斯山脉、阿尔卑斯山脉以及落基山脉上的冰川也消失了。
All sea ice is gone from both poles; mountain glaciers are gone from the Andes, Alps and Rockies.
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