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中国沙漠 ›› 2017, Vol. 37 ›› Issue (1): 158-166.DOI: 10.7522/j.issn.1000-694X.2015.00212

• 天气与气候 • 上一篇    下一篇

1961-2012年北疆干旱时空变化

吴燕锋, 巴特尔·巴克, 罗那那   

  1. 新疆农业大学 草业与环境科学学院, 新疆 乌鲁木齐 830052
  • 收稿日期:2015-07-27 修回日期:2015-09-30 出版日期:2017-01-20 发布日期:2017-01-20
  • 作者简介:吴燕锋(1986-),男,河南沈丘人,硕士研究生,研究方向为干旱区生态与环境。E-mail:wyfecology@163.com
  • 基金资助:
    国家国际科技合作计划项目(2010DFA92720-13);新疆研究生科研创新项目(XJGRI2014079);新疆维吾尔自治区土壤学重点学科项目

Spatiotemporal Pattern of Drought in North Xinjiang, China in 1961-2012

Wu Yanfeng, Bake Batur, Luo Nana   

  1. College of Grassland and Environmental Science, Xinjiang Agricultural University, Urumqi 830052, China
  • Received:2015-07-27 Revised:2015-09-30 Online:2017-01-20 Published:2017-01-20

摘要: 基于北疆38个气象站1961-2012年逐日的气象数据和综合气象干旱指数,探究了北疆干旱的时空演变特征。结果表明:1961-2012年,北疆旱情有所缓解,但干旱仍然频发,且全域性干旱较多,其中夏旱和秋旱较多且覆盖范围较大。干旱频次和干旱覆盖范围呈减少趋势,干旱强度逐渐减弱。四季中,冬季干旱缓解最为明显,其次是春季和夏季,秋季干旱略有缓解。空间上,自东南和东部向西北,旱情逐渐减轻。干旱强度和干旱频次中南部减势最明显,干旱频发会有所改善;东部减势较弱,干旱频发将会持续;西北部减势最弱,旱情仍持续较轻。气候变化下,北疆降水量和潜在蒸散量分别与综合气象干旱指数存在显著的正相关和负相关,北疆降水量的增加趋势和潜在蒸散量的减少趋势对北疆干旱缓解有重要的作用。

关键词: 北疆, 干旱, 时空变化, 气候因子

Abstract: The spatiotemporal pattern of drought in North Xinjiang of China from 1961 to 2012 was analyzed with daily meteorological data and compound index of meteorological drought. The results indicated that drought severity relieved by decreasing trend of drought coverage, frequency and intensity in North Xinjiang. However, the whole drought also happened frequently in summer and autumn in North Xinjiang. The drought severity alleviated most significantly in winter, followed by spring and summer, less significantly in autumn. The drought severity decreased from southeast to northwest in North Xinjiang. The spatial distribution of change trend of drought frequency and intensity indicated that drought severity relieved significantly in south and central region of North Xinjiang. Moreover, the precipitation and evapotranspiration had significantly positive and negative correlation with the value of compound index of meteorological drought, respectively. The increasing trend of precipitation and the decreasing trend of evapotranspiration have very impotent contribution to the alleviation of drought severity in North Xinjiang.

Key words: North Xinjiang, drought, spatiotemporal pattern, climate factors

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