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中国沙漠 ›› 2010, Vol. 30 ›› Issue (2): 452-460.

• 天气与气候 • 上一篇    下一篇

近51 a山西大风与沙尘日数的时空分布及变化趋势

苗爱梅1, 贾利冬2, 武 捷3

  

  1. 1.山西省气象台, 山西 太原 030006; 2.山西省气象局, 山西 太原 030002; 3.山西省气象信息中心, 山西 太原 030006
  • 收稿日期:2008-08-23 修回日期:2008-12-04 出版日期:2010-03-20 发布日期:2010-03-20

Space-Time Distribution and Changing Trend of Gale and Sand-Dust Days during Recent51 a in Shanxi

MIAO Ai-mei1, JIA Li-dong2, WU Jie3   

  1. 1.Shanxi Meteorological Observatory, Taiyuan 030006, China; 2.Shanxi Meteorological Bureau, Taiyuan 030002, China; 3.Shanxi Meteorological Information Center, Taiyuan 030006, China
  • Received:2008-08-23 Revised:2008-12-04 Online:2010-03-20 Published:2010-03-20

摘要: 利用地面气象观测数据,以瞬时风速≥17.0 m·s - 1 或风力≥8级的大风日数和沙尘天气发生日数为指标, 分析了山西大风、沙尘天气的时空分布特征,沙尘天气的变化特点及趋势,并从现代气候变化、大气环流特征及大风日数变化等方面,初步探讨了沙尘天气日数变化的气候原因。分析结果表明,山西的沙尘暴、扬沙与大风日数具有同位相、一峰一谷的逐月变化特征,峰值均出现在4月,谷值均出现在8—9月。浮尘日数具有两峰两谷的逐月变化特征,主峰与主谷与大风出现的时间一致,次峰和次谷则分别出现在每年的12月和2月。大风日数的峰值分别是沙尘暴、扬沙日数峰值的8.39倍和2.31倍;大风日数的谷值分别是沙尘暴、扬沙日数谷值的83.3倍和18.98倍。沙尘暴、扬沙与大风日数均有北部多于南部的空间分布特征,浮尘则与大风相反具有南部多于北部的空间分布特征。山西的沙尘暴、扬沙总日数在20 世纪90年代初期以后比50年代到70年代初期分别减少了84.9%和77.1%。多沙尘日数年大气环流的经向度较强, 乌拉尔山高压脊偏强, 东亚大槽位置偏西且加深, 少沙尘日数年则相反。比较发现,沙尘暴、扬沙和大风日数的变化趋势有很好的一致性,线性相关系数分别达到0.80和0.82。这表明,山西沙尘暴和扬沙的变化趋势主要是随大风的变化而变化,高纬冷空气向南爆发的频数减少、势力偏弱、路径偏北导致山西风力条件的减弱是近51 a沙尘暴、扬沙发生频数下降的主要原因。

关键词: 大风日数, 沙尘日数, 时空分布, 变化趋势

Abstract: Based on ground meteorological observational data, and taking the days of instantaneous wind speed ≥17.0 m·s-1 or wind force scale ≥8 and the sand-dust weather days as indexes, the author analyzed the space-time distribution and the changing trend of gale and sand-dust weather in Shanxi. Besides, the causes of sand-dust weather change are discussed from aspects of modern climatic change, general circulation characters and gale frequency change. Main results are as follows: The temporal variations of sand-dust storm, sand-blowing days and gale frequency are synchronous, showing "one-peak and one-vale inner-year mode" with peak in April and vale in month from Aug. to Sep. Variation of dust-floating days shows " two-peak and two-vale inner-year mode" whose principal peak and vale appeare simultaneously with gale, and secondary peak and vale appeare differently on December and February. The peak value and vale value of gale frequency are respectively as 8.39 and 83.3 times of that of sand-dust storm and 2.31 and 18^98 times of that of sand-blowing days. As for spatial distribution, sand-dust storm, sand-blowing days and gale days are more in the north than in the sout of Shanxi, but the distribution of dust-floating days is opposite. Variation in time, the total days of sand-dust storm and dust-blowing weather after early 1900s has decreased by 84.9% and 77.1% of that in 1950s and 1970s respectively. In the years when sand-dust events frequently happened the meridionality of general circulation is much forceful, the Ural pressure ridge is slightly strong, the East Asia great trough lies by west and deepens, but in the less sand-storm events years the case is on the contrary. The changing trend of sandstorm and sand-blowing days had perfect coherence with that of gale, and their linear correlative coefficients differently reach to 0.80 and 0.82. The result indicates that gale is the controlling factor of sand-dust storm and dust-blowing weather days in Shanxi province. Causes for decrease of sand-dust storm and sand-blowing days in Shanxi province during 1957—2007 mainly lie in wind force weakness due to frequency decrease and force weakness of going southward cold air from high latitude.

Key words: gale days, sand-dust days, space-time distribution, changing trend

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