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Jiang Xue-Gong Shen Jian-Guo Liu Jing-Tao Chung Yong-Seung 《Water, Air, & Soil Pollution: Focus》2003,3(2):191-212
By using observational data and MM5, an observational analysisand numerical study was conducted on the synoptic condition of a severe dust storm that was caused by a Mongolian cyclone whichoccurred from 6 to 8 April 2001. Results illustrated thatthe cyclogenesis was due to the isentropic potential vorticity (IPV) advection in the upper troposphere and the terrain modifiedbaroclinicity in the mid-lower troposphere. The Altai-Sayan complex of mountains blocked the lower level cold air and made the isentropic surface sharply steep. When the air slid down along the isentropic surface the increasing of baroclinicity anddecreasing of stability blew up the vertical vorticity development.The formation of the dust storm was a result of a cyclonic cold front passing across the area. The occurrence of this dust stormwas closely related to the strong surface wind, which was accompanied by a cold front passing, rather than the cyclogenesis, itself. Hence, the reason for the pre-front dust storm formulation was the formation of heating convection. Reasons behind the formation of a black storm (visibilitylower than 50 m), which occurred in the mid-north part ofInner Mongolia, lay in several aspects. Firstly, in thisarea the surface wind was strong, a direct result of thedownward transport in mid-lower troposphere. Secondly,the cold front passed over the effected area near sunsetso the air obtained much more surface heating to form adeeper mixed layer (ML). Thirdly, cooperation between thelower level wind and the terrain made the atmosphere inthis area and acquired the maximum advective contributionnecessary to form a deep post-front ML. The sensitivityexperiment revealed that surface heat flux was important to the frontal lifting. In addition, the forcing of surface heating wasalso seen as the primary forcing mechanism of frontogenesis. Meanwhile, removal of the surface heat flux made the atmosphericstratification became stable and the pre-storm ML very shallow,which weakened the strength of the dust storm. 相似文献
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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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Foreword Inglobalview ,droughtdisasterisregardedasthemostserioustypeofnaturaldisasterintheworld ,whichhascausedthewidestrangeofeffectsandthebiggesteconomiclosses .Se veredroughtsmainlyoccurinAfrica ,India ,China ,formerSovietUnion ,NorthAmerica ,andAustralia,accountingforalmosthalfofcountriesintheworld .Droughtdisasteroccursfre quentlyinChina ,withwiderangeofinfluence ,whichisthemostseriousmeteorologicaldisas ter ,causingeconomiclossesinagriculture .Fromthe 50’stothe 80’sinthe 2 0thcent… 相似文献
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紫露草微核技术对工业废水监测的应用 总被引:3,自引:0,他引:3
利用紫露草微核技术,以自来水为对照,不同浓度的氯化汞、三氧化二砷溶液及十几个工厂废水进行微核效应比较试验,筛选出破坏遗传物质的工业废水及其相应的污染水平。观察紫露草微核率变化及细胞的分裂情况,证明紫露草微核技术是监测工业废水的良好方法。 相似文献
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本文论述了在师专开展环境教育的意义和多维功能作用。总结了乐山师专长期肾开展环境教育的经验和特点,对全面提高学生素质,培养中学教改急需的环境教育师资具有重要的现实意义。 相似文献
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洗涤法处理含油土壤的研究 总被引:12,自引:1,他引:12
研究了用洗涤法处理含油土壤,考察了洗涤剂种类与浓度、洗涤温度、液固比、洗涤时间、表面活性剂、洗涤液直接循环使用次数对洗涤效果的影响,结果表明:当混合减浓度为10000mg/L、洗涤温度为70℃、液固比2:1、洗涤时间20min时,可将含油量为30%的土壤洗至残油率仅为0.3%左右。OP、EL型表面活性剂的加入对洗涤效果没有改善,特别有意义的是洗涤液能够直接循环使用而对洗涤效果基本无影响,这不仅能够减少用水量,还可以大大减少废水的排放量,降低操作费用及废水处理费用。该洗涤法不涉及物质的相变过程,混合碱由廉价的无机碱和无机盐组成,故能量消耗低,处理费用也低,且洗脱下来的原油可回收。 相似文献
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