热带东太平洋海温冬、春季的冷暖变化程度，可以预示后期西北夏季降水的趋势变化。
The variation of the east tropical pacific SST in winter and spring is able to predict precipitation trend of North west of China next summer.
图中并未显示某地区的绝对温度，但是显示了同一地区与1951-1980年相比的冷暖变化。
The maps do not depict absolute temperature, but how much warmer or colder a region is compared to the norm for that same region from 1951-1980.
由于河流阶地是间歇性新构造抬升的产物，其形成阶段又与气候的冷暖变化相关，即冷期阶地陡坎形成，暖期阶地堆积物形成。
Because the river terrace is the result of interrupting neotectonic uplift and its forming stages are bound up with the geologic climate cold warm changes, I.
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