Abstract
A comparative analysis for detecting temperature and precipitation changes in the period 1960–2010 was conducted using data from 74 meteorological stations in China’s arid northwest. Significant increasing trends (P < 0.01) were revealed through the investigation, showing rates of 0.343 °C/10a and 6.07 mm/10a, which is higher than the global average. The winter temperature rate increased 0.486 °C/10a, while the summer temperature changed at a rate of 0.232 °C/10a. However, although precipitation increased 2.51 mm/10a in summer, it slowed in winter to a rate of 1.16 mm/10a. Regionally, the highest increasing rates of temperature and precipitation occurred in northern Xinjiang, and the lowest rates were recorded in southern Xinjiang and the Hexi Corridor. We found that, among the four seasons, winter saw the greatest temperature changes. We also found that the winter temperature in this region had a strong association with the Siberian High (correlation coefficient: R = − 0.715) and greenhouse gas emissions (R = 0.51).
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Chen, Y., Li, B., Xu, C. (2014). Climate System in Northwest China. In: Chen, Y. (eds) Water Resources Research in Northwest China. Springer, Dordrecht. https://doi.org/10.1007/978-94-017-8017-9_2
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