Shi Xinghe, Li Fengxia, Zhaxi Cairang, et al. The variation of snow-cover and snow disaster in Qinghai during 1961—2004. J Appl Meteor Sci, 2006, 17(3): 376-382.
Citation: Shi Xinghe, Li Fengxia, Zhaxi Cairang, et al. The variation of snow-cover and snow disaster in Qinghai during 1961—2004. J Appl Meteor Sci, 2006, 17(3): 376-382.

The Variation of Snow-cover and Snow Disaster in Qinghai During 1961—2004

  • Received Date: 2005-04-26
  • Rev Recd Date: 2006-03-01
  • Publish Date: 2006-06-30
  • Using the grid data of 500 hPa height field which is provided by the Natoinal Climate Center and the ground meteorological observation data of seven meteorological stations over the eastern Haixi and around Qinghai Lake (36°~38°N, 96°~101°E) during 1961—2004, the snow disaster's annual table and ground snow sequence is collected, the circulation characteristic of the snow disaster occurred in snowy year and none-snowy year over the eastern Haixi and around Qinghai Lake is analyzed, and based on the climatic diagnosis and the mathematical statistics method the interannual variation characteristic and the generating mechanism as well as the cause of snow disaster are studied. The result shows that the probability of the occurrence of the regional snow disaster over the eastern Haixi and around Qinghai Lake is 15.9% (7/44), while the probability of the occurrence of the local snow disaster is only 9.1% (4/44). Among the eleven snow disasters the probability of snow disaster is 91% (10/11) in later winter to spring (from January to April), and the probability is 9% (1/11) in early winter (from mid October to December). The slowly increasing of the accumulated snow-cover amount over the eastern Haixi and around Qinghai Lake in winter in the 44 years is prone to snow-cover and low temperature damage. The primary influencing system of precipitation over this region is the plateau trough, Mongolia trough and plateau low cyclone (at the same time accompanying convergence line and shearing line), i.e., when the 500 hPa polar vortex center of the north hemisphere from winter to spring is leaning against west/east hemisphere, or the height anomaly of Tibetan Plateau and eastern coast region forms into anomaly distribution with "low in west but high in east (or high in east but low in east)", there has more (only less) snow over the eastern Haixi and around Qing hai Lake. The variation trend of the snow-cover amount in winter and spring in the future 10 years is corresponded with the variation in 1990s, and it also keeps increasing. The snow disasters in later winter to spring over the eastern Haixi and around Qinghai Lake have relationships not only with the local weather and changing climate, but also with the local landform.
  • [1]
    张顺利, 陶诗言.青藏高原积雪对亚洲夏季风影响的诊断及数值研究.大气科学, 2001, 25 (3): 372-390. http://www.cnki.com.cn/Article/CJFDTOTAL-DQXK200103008.htm
    [2]
    陈乾金, 高波, 李维京, 等.青藏高原冬季积雪异常和长江中下游主汛期旱涝及其与环流关系的研究.气象学报, 2000, 58 (5): 582-595. http://www.cnki.com.cn/Article/CJFDTOTAL-QXXB200005006.htm
    [3]
    郑益群, 钱永甫, 苗曼倩, 等.青藏高原积雪对中国夏季风气候的影响.大气科学, 2000, 24 (6): 761-774. http://www.cnki.com.cn/Article/CJFDTOTAL-DQXK200006003.htm
    [4]
    陈乾金, 高波, 张强, 等.青藏高原雪盖异常与夏季风变异及其相互联系的物理诊断研究.大气科学, 2000, 24 (4): 477-492. http://www.cnki.com.cn/Article/CJFDTOTAL-DQXK200004004.htm
    [5]
    陈烈庭, 闫志新. 青藏高原冬春异常雪盖影响初夏季风的统计分析∥中长期水文气象预报文集. 北京: 水文电力出版社, 1981: 138-141.
    [6]
    陈烈庭, 闫志新. 青藏高原冬春异常雪对大气环流和我国南方汛期降水的影响∥中长期水文气象预报文集. 北京: 水文电力出版社, 1979: 185-194.
    [7]
    郭其蕴, 王继琴.青藏高原的积雪及其对东亚季风的影响.高原气象, 1986, 5 (2): 122-123. http://www.cnki.com.cn/Article/CJFDTOTAL-GYQX198602001.htm
    [8]
    徐国昌, 李珊, 洪波.青藏高原雪盖对我国环流和降水的影响.应用气象学报, 1994, 5 (3): 62-67. http://qikan.camscma.cn/jams/ch/reader/view_abstract.aspx?file_no=19940111&flag=1
    [9]
    李培基.高亚洲积雪分布.冰川冻土, 1995, 17 (4): 297-298. http://www.cnki.com.cn/Article/CJFDTOTAL-BCDT504.001.htm
    [10]
    韦志刚, 吕世华.青藏高原积雪的分布特征及其对地面反照率影响.高原气象, 1995, 14 (2): 67-73. http://www.cnki.com.cn/Article/CJFDTOTAL-GYQX501.007.htm
    [11]
    韦志刚, 黄荣辉, 陈文, 等.青藏高原地面积雪的空间分布和年代际变化特征.大气科学, 2002, 26 (4): 496-508. http://www.cnki.com.cn/Article/CJFDTOTAL-DQXK200204006.htm
    [12]
    周陆生, 李海红, 汪青春.青藏高原东部牧区大—暴雪过程及雪灾分布的基本特征.高原气象, 2000, 19 (4): 450-458. http://www.cnki.com.cn/Article/CJFDTOTAL-GYQX200004006.htm
    [13]
    董安祥, 瞿章, 尹宪志.青藏高原东部雪灾的奇异谱分析.高原气象, 2001, 20 (2): 213-219. http://www.cnki.com.cn/Article/CJFDTOTAL-GYQX200102016.htm
    [14]
    董文杰, 韦志刚, 范丽军.青藏高原东部牧区雪灾的气候特征分析.高原气象, 2001, 20 (4): 402-406. http://www.cnki.com.cn/Article/CJFDTOTAL-GYQX200104008.htm
    [15]
    马林, 李锡福, 张青梅, 等.青藏高原东部牧区冬季雪灾天气的形成及其预报.高原气象, 2001, 20 (3): 325-331. http://www.cnki.com.cn/Article/CJFDTOTAL-QHQX200304001.htm
    [16]
    黄嘉佑.气候状态变化趋势与突变分析.气象, 1995, 21 (7): 46-59. http://www.cnki.com.cn/Article/CJFDTOTAL-QXXX507.011.htm
    [17]
    陈隆勋, 朱文琴, 王文.中国近45年气候变化的研究.气象学报, 1998: 56 (5), 257-271. http://www.cnki.com.cn/Article/CJFDTOTAL-QXXB803.000.htm
    [18]
    史国枢.青海自然灾害.西宁:青海人民出版社, 2003: 150-160.
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    • Received : 2005-04-26
    • Accepted : 2006-03-01
    • Published : 2006-06-30

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