4.5 Article

Temperature and precipitation long-term trends and variations in the Ili-Balkhash Basin

期刊

THEORETICAL AND APPLIED CLIMATOLOGY
卷 115, 期 1-2, 页码 219-229

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SPRINGER WIEN
DOI: 10.1007/s00704-013-0883-3

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资金

  1. Ministry of Water Resources' Special Funds for Scientific Research on Public Causes, People's Republic of China [201001052]
  2. Major program of National Social Science Foundation of China [11ZD168]
  3. Innovative Project of Scientific Research for Post-graduates in Ordinary Universities in Jiangsu Province [CX09B_161Z]
  4. Cultivate Project for Excellent Doctoral Dissertation in Hohai University, Fundamental Research Funds for the Central Universities [2010B18714]

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This study analyzed the long-term trends and variations of temperature and precipitation on annual timescale in the Ili-Balkhash Basin (IBB), Kazakhstan. Some statistical tools were employed to detect any climate variations at four stations in the IBB during the period between 1936 and 2005. These methods included the Mann-Kendall trend test, the Theil-Sen approach, and the sequential Mann-Kendall test. The results showed that in temporal scale, the climate in the IBB has been becoming warmer and wetter in the past several decades as a whole. The annual mean temperature and the annual precipitation in the IBB showed an increasing trend since the 1970s and the 1940s, respectively. The significance of the annual mean temperature and annual precipitation trends in the IBB was tested at > 95 % confidence level. The slope of the increasing trend of annual mean temperature ranges from 0.019 to 0.029 A degrees C/year, and that of the annual precipitation ranges from 0.654 to 2.179 mm/year. In spatial scale, the multiyear mean values of temperature and precipitation are greater in the southern mountain region than those in the northern plain and hilly land area of the basin. The multiyear mean temperature decreases with the increasing latitudes, while increases with the increasing altitudes except for Karaganda; the multiyear mean precipitation increase with the increasing altitudes, while decreases centered with the Lake Balkhash from the surrounding area. The results may provide climatic backgrounds for solving the problems related to water sources of the IBB.

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