Climate Change Research ›› 2018, Vol. 14 ›› Issue (6): 562-572.doi: 10.12006/j.issn.1673-1719.2018.061

• Changes in Climate System • Previous Articles     Next Articles

Spatial variation of humidity and its influencing factors in the north and south slopes of the Tianshan Mountains, China during 1966-2015

Di-Tao CHEN1,2,Fa-Rong HUANG1,3,Qian LI1,2,Lan-Hai LI1,3,4,5   

  1. 1 State Key Laboratory of Desert and Oasis Ecology, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China
    2 University of Chinese Academy of Sciences, Beijing 100049, China
    3 Ili Station for Watershed Ecosystem Research, Chinese Academy of Sciences, Urumqi 830011, China
    4 Xinjiang Regional Center of Resources and Environmental Science Instrument, Chinese Academy of Sciences, Urumqi 830011, China
    5 Research Center for Ecology and Environment in Central Asia, Chinese Academy of Sciences, Urumqi 830011, China
  • Received:2018-04-25 Revised:2018-07-14 Online:2018-11-30 Published:2018-11-30
  • Contact: Lan-Hai LI

Abstract:

Daily meteorological data during 1966-2015 were used to analyze the spatio-temporal distribution characteristics of relative humidity (RH) in the north and south slopes of the Tianshan Mountains by using Mann-Kendall trend test. In addition, sensitivity coefficient and relative contribution were calculated to assess the impact of temperature, precipitation, reference evapotranspiration, wind speed and sunshine duration on RH. The results revealed that RH in the north slope exhibited fluctuating downward trend, but in the south slope it showed the opposite trend. Furthermore, the RH showed a rising gradient from south to north slope. As for seasonal RH, an upward trend was found in summer, autumn and winter, but a downward trend was observed in spring in the entire Tianshan Mountains. Sensitivity analysis indicated that RH was negatively related to temperature, reference evapotranspiration, wind speed and sunshine duration, but positively related to precipitation. Moreover, RH was the most sensitive to sunshine duration, reference evapotranspiration and wind speed, but precipitation was most insensitive, whether in north or south slope. Spatially, the high value area of sensitivity coefficient of precipitation was located in the Ili Valley, while others were located in the south slope. Contribution analysis suggested that the impact of reference evapotranspiration on RH was much larger than other factors. The high contribution area of sunshine duration was distributed in the Ili Valley (north slope), but that of wind speed, precipitation and temperature in Kizilsu (south slope).

Key words: North and south slopes of the Tianshan Mountains, Relative humidity (RH), Differences, Mann-Kendall trend test, Sensitivity analysis

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