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121.
122.
Oliveira Amauri P. Bornstein Robert D. Soares Jacyra 《Water, Air, & Soil Pollution: Focus》2003,3(5-6):3-15
The major topographic, mesoscale, and urban influences on the wind patterns of the City of São Paulo are characterized using one year of surface wind velocity data observed at 11 surface stations within its urban limits. The data was used to study the diurnal and annual variations of wind velocity and horizontal wind divergence within the city. Results showed that the circulation over the investigated area is dominated by three major factors: sea breeze; mountain-valley circulations; and urban effects, such as roughness, building-barrier, and urban heat island. The sea breeze was found to be the dominant feature of the monthly-averaged diurnal variation of São Paulo surface winds during the eight warmest months of the year. The sea breeze front induces a velocity minimum at the time of its passage and a post-frontal afternoon velocity maximum. Mountain-valley thermal effects on the flow can be seen in the temporal divergence/convergence patterns. These thermal effects tend to be more important during colder months, at night, and when the wind velocities are low. Nighttime downslope convergent flows are present over the city during winter and spring and daytime upslope divergent flows are present over the city during summer months. 相似文献
123.
Occurence and Distribution of Polycyclic Aromatic Hydrocarbons in Ankara Precipitation 总被引:1,自引:0,他引:1
Urban atmospheric environment contains many trace organic pollutants that are related to the incomplete fuel combustion in domestic heating, industrial plants and automobile traffic. Removal of these pollutants from the atmosphere takes place through wet and dry deposition as well as chemical transformations. In this study, concentrations of polycyclic aromatic hydrocarbons (PAHs) in wet deposition samples were determined at an urban site of Turkey. Wet and dry deposition samples were collected using Andersen Rain Sampler. The sampler was modified accordingly for the collection of organic pollutants. Collected samples were preconcentrated by using solid phase extraction (SPE) disks and consecutively analyzed by Gas Chromatography-Mass Spectrometry (GC-MS). Among the 13 compounds quantified in this study, anthracene, fluoranthene, and pyrene were found more frequently and at elevated concentrations (202, 271 and 260 ng L-1 mean concentrations, respectively).Concentrations of PAHs were found to be high in winter period. 相似文献
124.
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
125.
126.
土地利用变化驱动下的上海市区水灾灾情模拟 总被引:14,自引:0,他引:14
对上海市区近50年来的土地利用结构变化进行了重建,并计算了由土地利用变化引起的上海市区水位变化量。以特定的1962年水灾为参照,模拟在同等雨强情况下,由土地利用结构变化和地面沉降引起的淹没范围的变化以及由此带来的水灾损失的变化。结果表明,在49mm/d降水条件下,由于土地利用的变化,使2001年的径流系数比1950年增大了34.0%,2001年的水位比1950年增高了45.9%;2001年的水灾灾情为1950年的1.0629倍;即使在目前千年一遇的防洪标准下,亦可造成相当于2001年地均GDP值0.088%(约为4.5亿元人民币)的损失,这是1991年相应数值的220倍。 相似文献
127.
浙江城镇空间扩展与经济发展的遥感研究 总被引:1,自引:0,他引:1
近年来。浙江省经济飞速发展。城镇规模迅速扩大。但有关全省城镇建成区扩展面积的具体数量和扩展速度的客观数据还很缺乏。利用多时相的Landsat卫星遥感图像数据。采用目视解译与计算机自动分类方法,对1998~2001年浙江省城镇时空扩展进行了调查。调查结果显示,1998年和2001年浙江省县级以上城市建成区面积分别为977.85km^2和1499.06km^。3年内全省县级以上城市建成区面积扩展了521.21km^2,年增长速率达15.31%。在此基础上,根据区域社会经济统计数据,对城镇经济发展与城市空间扩展的相关性进行了分析。 相似文献
128.
西北地区沙尘暴引发的荒漠化问题 总被引:4,自引:2,他引:4
从西北地区继1993~1995年连续3a出现沙尘暴之后,1996年甘肃和内蒙古西部的阿盟等地再次遭到沙尘暴的袭击入手,分析了沙尘暴发生的原因,指出它归根结底是荒漠化的直接后果。概述了荒漠化的状况及危害,并分析了其成因。 相似文献
129.
Christopher R. Ellis Jerry Champlin Heinz G. Stefan 《Journal of the American Water Resources Association》1997,33(6):1363-1374
ABSTRACT: Evidence is presented that snowmelt runoff from an urban watershed can produce density current intrusions (underflows) in a lake. Several episodes of density current intrusions are documented. Water temperatures and salinities measured near the bottom of a 10 m deep Minneapolis lake during the late winter warming periods in 1989, 1990, 1991, and 1995 show significant rapid changes which are correlated with observed higher air temperatures and snowmelt runoff. The snowmelt runoff entering this particular lake (Ryan Lake) has increased electrical conductivity, salinity, and density. The source of the salinity is the salt spread on urban streets in the winter. Heating of littoral waters in spring may also contribute to the occurrence of the sinking flows, but is clearly not the only cause. 相似文献
130.
侯祺棕 《中国安全科学学报》1996,6(3):1-5
矿山呼吸性粉尘危害程度评价法研究侯祺棕(武汉工业大学资源与环境工程系)[摘要]通过对矿山呼吸性粉尘实际危害程度评价法的研究,并经实例检验,推荐两种具有可操作性和足够准确的评价法,这对矿山呼吸性粉尘监测新技术的推广具有重要意义。[关键词]呼吸性粉尘,危... 相似文献