然而，温度的波动引起冰川增长和消融。
However, temperature fluctuations have caused glacier growth and depletion.
我们已经注意到温度的波动情况。
年降水量和年平均温度的波动特点是决定累加作用时间和影响强度的关键。
The variation of air mean temperature and annual precipitation played a key role in the duration and intensity of cumulative impacts on desertification.
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