摘要
对1961—2010年淖毛湖气象站沙尘暴资料的分析表明,沙尘暴主要出现在3—5月,4月份最多;沙尘暴天气主要集中在白天,占总次数的83%,夜间相对较少,只占17%。50年内淖毛湖出现沙尘暴天气过程804次,以西方和西北方冷空气入侵为主,集中发生在3—5月;50年来淖毛湖沙尘暴日数呈减少趋势,按线性拟合其减少率为0.711 d/10 a。20世纪60年代中期到70年代沙尘暴日数呈现急剧增加趋势,1974年沙尘暴日数多达54 d,20世纪80年代后沙尘暴日数呈现急剧下降趋势,年日数减少到1 d,甚至个别年份未出现沙尘暴天气,该时期大风日数减少、风力强度减弱是主要原因外,生态环境改善,局地植被增加也是重要因素。
Through analyzing sand-storm data of Naomao Lake Weather Sta-tion from 1961 to 2010, sandstorm main-ly occurred from March to May, especial-ly in April;sandstorm mainly occurred in the daytime (accounting for 83% of the total), and less at night (only 17% of the total). Within the half century, 804 sand-storms occurred in the region of the Naomao Lake, especially cold air invad-ed from west and northwest from March to May;the sandstorm days in this region reduce, and the reduction rate of the lin-ear fitting was 0.711 d/10 a. From the middle 1960s to the 1970s, sandstorm days increased drastically, achieved 54 days in 1974; sandstorm days reduced sharply since the 1980s, by 1 day annu-ally, even no sandstorm occurred in some years, because heavy wind days and wind strength reduced, ecological environment improved, and regional veg-etation increased.
出处
《农业灾害研究》
2014年第12期44-46,共3页
Journal of Agricultural Catastrophology
关键词
沙尘暴
时空分布
变化趋势
Sandstorm
Temporal-spatial distribution
Change tendency