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Wang Xu Ma Yu Chen Hongwu Wen Gang Chen Shoujun Tao Zuyu Chung Yong-Seung 《Water, Air, & Soil Pollution: Focus》2003,3(2):67-79
With observational data spanning 1961–1999 from 90 meteorological stations in Xinjiang, China, the spatial and temporal characteristics of sandstorms and strong winds, and the contribution of strong winds to the occurrence of sandstormsare analyzed. Moreover, the dominant wind direction and minimumwind speeds during sandstorm periods are discussed. The research shows that although possessing similar climatic trends, sandstorms and strong winds in Xinjiang have opposite geographical distributions, i.e. places with more sandstorms show fewer strong winds. The contribution of strongwinds to sandstorms in northern Xinjiang is larger than that insouthern Xinjiang. The dominant wind directions clearly indicatethe paths of the weather systems that introduced the sandstorms.The minimum wind speeds in the sandstorms were over 10 ms-1in northern and eastern Xinjiang and in the Turpan and Yanqi Basins of southern Xinjiang. In Tarim Basin of southern Xinjiang,however, the minimum wind speed was about 6–8 ms-1, and even 6 ms-1 at its southern edge. 相似文献
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北京市与香河县大气臭氧及氮氧化合物的变化特征 总被引:2,自引:1,他引:2
于2005年春、夏之交,在北京市及河北省香河县两地同时开展了臭氧和氮氧化合物的连续监测.结果表明,香河县和北京市的臭氧统计日变化形式基本一致,北京市大气臭氧平均浓度比香河低,分别为28×10-9V/V和43×10-9V/V;大气中0x浓度北京市高于香河县,分别为72×10-9V/V和60×10-9V/V.观测期间,两地臭氧的月最高值出现时间一致,其中6月21日北京市的臭氧浓度最高达到200×10-9V/V,香河县也达到149×10-9V/V.在三次臭氧严重超标事件发生的前一天,两地都伴随有氮氧化合物的高浓度积累;南风时北京市和香河县的Ox浓度都比平均值高25%. 相似文献
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农业经历了生态农业、化学农业到生态农业的变迁,生态农业是起点也是终点。发达国家饱尝了发展化学农业的苦果,随后转轨到生态农业的道路上,最后认识到只有发展循环农业才能够做到农业可持续发展。发达国家的循环农业特别强调生态内涵和变废为宝理念,政府的财政投入和科研投入力度很大。相比之下,我国虽然已经开始发展循环农业,但目前还并不普遍,化学农业还占有很大比例。学习吸收发达国家的经验,会让我国尽早走上循环农业的发展道路。循环农业是我国农业的发展方向,为了做到这一点,需要强化农业产业化力度、加大财政补贴力度和科研投入力度。 相似文献
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N. Foroud R. S. Broughton G. L. Austin 《Journal of the American Water Resources Association》1984,20(1):87-91
ABSTRACT: The effects of a moving rainstorm on flood runoff characteristics were investigated. A flood hydrograph simulation model called “FH-Model” and a natural watershed were used. A hypothetical rainstorm of 50 years recurrence interval, 75 mm depth, and 4 hours duration was used to show the effects of velocity and direction of the moving rainstorm on the runoff characteristics. Compared with an equivalent stationary rainstorm (ESRS), the peak flow caused by a rainstorm moving in a downstream direction with a speed equal to channel velocity, V, was 27.5 percent higher and the peak flow caused by the same rainstorm moving in an upstream direction was 21.7 percent smaller. These percentages reduced to 10.5 percent and 8.6 percent for storms moving downstream and upstream, respectively, at three times the channel velocity, 3V. There were negligible differences in the time of peak, Tp between runoff caused by storms moving downstream and runoff produced by ESRS. However, Tp for a storm moving upstream at V velocity was 82 percent higher than that produced by ESRS, but was reduced to 27 percent higher when the storm velocity was 3V. 相似文献