但是所有人都认为地中海和孟加拉湾过高的水面温度导致了过多的水分进入大气。
But all agree that the excessive amount of moisture pumped into the atmosphere is a result of high water surface temperatures in the Mediterranean and Bay of Bengal.
总体上2010年和2005年的地表温度比20世纪的平均温度高了1.12华氏度（0.62摄氏度），其中包括世界各地的陆地及水面温度。
Overall, 2010 and 2005 were 1.12 degrees Fahrenheit (0.62 Celsius) above the 20th-century average when taking a combination of land and water surface temperatures across the world, it said.
冰减少的越多，形成的无冰水面就会越多，这些无冰水面在夏天时的温度会持续升高，在冬天结的冰就会减少，来年夏天也会有更多的冰融化。
The more you lose, the more open water is created, the more warming goes on in that open water during the summer, the less ice forms in the winter, the more melt there is the following summer.
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