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气温突变后内蒙古气候显著变暖，与突变前相比有明显差异。
After the abrupt change of temperature, the climate of Inner Mongolia was warming obviously, compared with abrupt change before, there was obvious difference.
秦岭南北降水突变年份大多早于气温突变年份，相关机理仍待进一步研究。
The precipitation abrupt change came earlier than that of temperature in both southern and northern Qinling Mountains. The related reasons remain to be further discussed, nevertheless, it inspired us.
各个季节(冬李除外)及年气温突变性增温主要发生在夜间，且在前期夏季白天气温发生跃变性降温。
Seasonal and annual temperature "s paroxysmal increase mainly happen at night, and the summer daytime temperature has paroxysmal decrease in the early stage."
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