气候变化研究进展 ›› 2012, Vol. 8 ›› Issue (5): 364-371.doi: 10.3969/j.issn.1673-1719.2012.05.008

• 中国冰川资源专栏 • 上一篇    下一篇

中国积雪时空变化分析

刘俊峰1,2,陈仁升1,2,宋耀选1,2   

  1. 1. 中国科学院寒区旱区环境与工程研究所黑河上游生态-水文试验研究站
    2. 内陆河流域生态水文重点实验室
  • 收稿日期:2012-02-02 修回日期:2012-05-08 出版日期:2012-09-30 发布日期:2012-09-30
  • 通讯作者: 刘俊峰 E-mail:jfliu121@163.com
  • 基金资助:

    全球变化研究国家重大科学研究计划项目“北半球冰冻圈变化及其对气候环境的影响与适应对策”(2010CB951401);国家自然科学基金项目(91025011;40771045)共同资助

Distribution and Variation of Snow Cover in China

  • Received:2012-02-02 Revised:2012-05-08 Online:2012-09-30 Published:2012-09-30
  • Contact: LIU Jun-Feng E-mail:jfliu121@163.com

摘要: 结合2001—2010年Aqua与Terra卫星MODIS积雪影像,分析了新疆、青藏高原和东北-内蒙地区积雪的空间稳定性,并探讨了这三大积雪区积雪季节和年际变化特征。结果表明,三大积雪区中新疆积雪空间稳定性最好,东北-内蒙地区次之,青藏高原较差,其稳定性指数分别为0.58、0.38和0.29。三大积雪区积雪年内分配存在显著的季节特征,2001—2010年新疆和东北-内蒙积雪区积雪面积最大值一般出现在1月,偶尔出现在12月,到7月和8月积雪面积很小;青藏高原积雪面积最大值则有可能出现在11—2月,其中以11月出现频率最高,10—3月的积雪面积差异相对其他两个积雪区的变化较小。从年际变化上看,2002年以来三大积雪区及全国稳定积雪面积无明显变化。

关键词: 积雪日数, 空间分布, MODIS, 季节及年际变化

Abstract: New snow cover products were produced by the combined using of Aqua and Terra MODIS snow cover products in 2001-2010. Then the distribution and variation of snow cover over the three major snow-covered regions in China were studied. The outcome shows that Xinjiang region’s snow cover is more stable than Northeast China-Inner Mongolia region’s and Tibetan Plateau’s. The corresponding stable indices of snow cover over the three regions are 0.58, 0.38 and 0.29, respectively. The seasonal snow-covered areas in different month were also studied, which shows that in Xinjiang and Northeast China, the largest snow-covered area appeared in January, and the smallest in July and August. In Tibetan Plateau, the largest snow-covered area appeared in November, after then the area reduced gradually till April, afterwards quickly till July and August. The yearly stable snow-covered area has not significantly changed over three major snow-covered regions and entire China since 2002.

Key words: snow cover days,  , spatial distribution, MODIS, seasonal and yearly variations

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