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中国农学通报 ›› 2014, Vol. 30 ›› Issue (20): 223-228.doi: 10.11924/j.issn.1000-6850.2013-2518

所属专题: 农业气象

• 资源 环境 生态 土壤 气象 • 上一篇    下一篇

西藏冰雹日数的时空分布特征

路红亚 林志强 洪健昌   

  • 收稿日期:2013-09-24 修回日期:2013-10-30 出版日期:2014-07-15 发布日期:2014-07-15
  • 基金资助:
    自然科学基金(41165011)。

Characteristics of Spatial-temporal Distribution About Hail Days Over Tibet

  • Received:2013-09-24 Revised:2013-10-30 Online:2014-07-15 Published:2014-07-15

摘要: 为了全面、深入地了解西藏冰雹天气分布特征以及变化趋势,为政府和社会有关部门防灾减灾提供科学依据。笔者基于1981—2010年西藏38个台站的冰雹观测资料,分析了冰雹日数的时空变化特征,发现全区冰雹日数呈东南向西北递增分布,年平均冰雹日数在10天以上的区域主要分布在海拔4000 m以上的浪卡子及高原北部区域,冰雹频发区主要集中在那曲地区。对西藏高原冰雹日数进行EOF分析,表明高原冰雹日数存在着“整体一致型”、“南北差异型”2种空间分布型。每天12—21时是西藏冰雹集中时段,尤其是午后至傍晚尤为显著。全年降雹主要集中在6—9月,其中有6成以上发生在夏季,而11月及整个冬季的雹日不足1天。西藏年雹日呈线性减少趋势的站点明显多于呈线性增加的站数,年雹日具有显著的减少趋势,平均每10年减少7.7天。

关键词: 生长状况, 生长状况

Abstract: For a comprehensive, in-depth understanding of the characteristics and distribution of Tibetan hail trends relevant for the government and society to provide a scientific basis for disaster prevention and mitigation. The author used the method of Empirical Orthogonal Function (EOF), the characteristics of spatial-temporal distribution about hail days were analyzed based on the daily hail records of 38 stations over Tibet during 1981 to 2010. Results showed that hail days over Tibet increased from southeast to northwest part of Tibet, and the area with annual average hail days more than 10 days was distributed in Langkazi and north region of the Tibet Plateau above 4000 m sea level. There were 2 spatial distribution characteristics about hail days: unitary consistency, difference between south and north in Tibet. The hail occurred frequently at 12-21 o’clock, especially during afternoon to dusk and often occurs in June to September especially in summer with 60% hail occurrence, but in winter not enough 1 days in Tibet. The annual hail days decreased significantly with the rate of 7.7 d/10 a.