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干旱区地理 ›› 2013, Vol. 36 ›› Issue (6): 1013-1022.

• 气候与水文 • 上一篇    下一篇

新疆阿勒泰地区冬季大到暴雪气候变化特征

庄晓翠1,李博渊2,张林梅1,杨森1,白松竹1,王海岩2   

  1. (1    新疆阿勒泰地区气象局,新疆    阿勒泰    836500;    2    新疆青河县气象局,新疆    青河    836200)
  • 收稿日期:2013-01-06 修回日期:2013-03-11 出版日期:2013-11-25
  • 作者简介:庄晓翠(1964-),女,重庆人,本科,高级工程师,从事天气预报、气候变化及其相关的研究工作. Email:zxcxjalt@163.com
  • 基金资助:

    公益性行业科研专项“新疆北部致灾暴雪成因分析和预报技术研究”(GYHY201106007);气候变化对西北干旱区水循环影响机理与水资源安全研究2010 CB951001

Heavy snowstorm characteristics of climatic change in winter in Altay Xinjiang

ZHUANG  Xiao-cui1,LI  Bo-yuan2,ZHANG  Lin-mei1,YANG  Sen1,BEI  Song-zhu1,Wang Hai-yan2   

  1. (1   Xinjiang of Aletai Meteorological Bureau, Aletai  836500, Xinjiang, China;2   Xinjiang of Qinghe Meteorological Bureau, Qinghe  836200, Xinjiang, China)
  • Received:2013-01-06 Revised:2013-03-11 Online:2013-11-25

摘要: 基于新疆阿勒泰地区7个观测站1961-2010年冬季逐日降水量资料,定义了大到暴雪特征量,并对其时间序列进行标准化,然后运用线性趋势、Cubic函数、M-K突变检验、Morlet小波变换、R/S分析等方法,研究了该区冬季大到暴雪的气候变化特征。结果表明:大到暴雪量对冬季降水总量的方差贡献较大。在气候分布上,大到暴雪特征量、冬季总降水量的大值区均位于北部东部,大值中心位于富蕴或阿勒泰站,方差贡献大值中心位于青河站;小值中心位于福海站。在年际尺度上,该区各特征量有7 a的显著周期变化特征;在年代际尺度上,有13~15 a、17~23 a、28~29 a的显著周期变化。在时间域上,大到暴雪量和频次在20世纪90年代之前以负距平为主,变化相对平稳,90年代之后以正距平为主,变化相对剧烈;大到暴雪强度60-70年代初、80年代中期到21世纪最初10 a波动幅度较大,70年代中期到80年代初变化相对平稳。Cubic函数拟合表明,大到暴雪特征量在80年代末90年代初发生了由少到多的转型,但没有突变点。在空间域上,各年代大到暴雪量大值区所在范围比较稳定,位于北部东部,小值区出现在河谷平原;值中心在60和90年代出现在富蕴站,其它年代出现在阿勒泰站;小值中心70年代出现在布尔津站,其它年代均出现在福海站;大到暴雪频次的变化与其不同的是大值中心90年代出现在青河站;大到暴雪强度在60和70年代大值中心位于阿勒泰站,80和90年代位于富蕴站,21世纪最初10 a位于哈巴河站,大值区分布也较复杂。大到暴雪特征量全区及各站均呈增多趋势;大到暴雪量是阿勒泰和福海站、大到暴雪频次和强度是阿勒泰、福海、富蕴站没有通过显著性检验,其它均通过了显著性检验。R/S分析表明,在未来该地区大到暴雪特征量将逐渐转为减少的趋势,尤其是吉木乃站。通过分析揭示了阿勒泰地区大到暴雪变化规律,对指导该地区经济生产布局、防灾减灾、暴雪灾害风险评估提供参考,同时也为短期气候预测提供依据。

关键词: 新疆阿勒泰, 冬季, 大到暴雪, 气候变化特征

Abstract: Based on the global warming background,this paper studied heavy snowstorm climate characteristics in the Altay prefeture,revealed variation law of heavy snowstorm in this prefecture,and provided reference for guiding the region economy layout,disaster prevention and mitigation,blizzard disaster risk assessment. And at the same time,this paper provided the basis for the short-term climate prediction. It used the daily precipitation data of 1961-2010 winters at seven observation stations of the Altay prefecture,defined the heavy snowstorm characteristics,and standardized the time series. With the help of Linear Trend Method,Cubic function,Mann-Kendall mutation testing,Morlet wavelet transform and R/S analysis,the heavy snowstorm characteristics of climatic change in winters.were studied.  The results show that: the total rainfall of heavy snowstorm contributes great value to the variance of the total rainfall in winters.  In the climatic distribution,the large value area of heavy snowstorm characteristic quantity and the total rainfall in winters locates in its northern and eastern parts with the large value center laying at Fuyun or Altay station,variance contribution value center at Qinghe station. Small value center locates at Fuhai station. On an inter annual scale,each characteristic quantity has 7 a periodic variation characteristics in this prefecture; In view of the inter-decadal scale,significant periodic variations are 13-15 a,17-23 a,and 28-29 a. In the time domain,rainfall and frequency of heavy snowstorm were characterized by negtive anomaly before the 1990s,change was relatively smooth,and by positive anomaly after the 1990s,and change was relatively acute. The heavy snowstorm intensity fluctuated greatly from 1960s to 1990s begining and from the mid-period of 1980s to the 2000s,the change in intensity was relatively smooth from the mid-period of the 1970s to the 1980s beginnig. The cubic function fitting shows that: The heavy snowstorm characteristics produced a type transformation from less occurrence to much occurrence in late 1980s and early 1990s,but there was no mutation point. In the spatial domain,the location of heavy snowstorm’s large value area was relatively stable for every decade,locating in the north and eastern,small value area appeared in valley and plain. Large value center appeared at Fuyun station in 1960s and 1990s,and appeared at Altay station in the other decades; small value center appeared at Buerjin station in the 1970s,and appeared at Fuhai station in the other decades. The change in frequency of the heavy snowstorm was different to the change in the large value center and appeared at Qinghe station in the 1990s; The heavy snowstorm intensity’s large value center lay at Altay station in 1960s and 1970s,at Fuyun station in 1980s and 1990s,at Habahe station in 2000s,and the large value area distribution was more complex. The heavy snowstorm characteristic quantity was with an increasing trend in the whole prefecture; the trend coefficients were 0.374,0.364 and 0.359; climate tendency was 0.22 mm/10 a,0.20 d/10 a and 0.16(mm/d)/10 a. Among these stations,the large heavy snowstorm amount appeared at Altay and Fuhai stations,the large frequency and intensity appeared at Altay and  Fuhai stations,and Fuyun station did not pass the significance test,the other stations passed the significance test. R/S analysis showes that the heavy snowstorm characteristic quantity would gradually be changed in a reduced tendency,especially at Jimunai station.

Key words: Altay Xinjiang, winter, heavy snowstorm, climate characteristic

中图分类号: 

  • P468.0.27