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161.
长江黄河源区多年冻土变化及其生态环境效应   总被引:29,自引:1,他引:29  
应用江河源区五站1980-1998年0cm、5cm、10cm、15cm、20cm、40cm浅层地温资料、钻孔深层地温资料以及勘探资料,详细分析了两大源区的冻土变化,结果表明:近20年来,受气候变暖影响,江河源区多年冻土总体上保存条件不利,区域上呈退化趋势。岛状多年冻土和季节冻土区年均地温升高约0 3~0 7℃,大片连续多年冻土区升幅较小,为0 1~0 4℃。多年冻土上限以2~10cm/a的速度加深。在黄河源多年冻土的边缘地带,垂向上形成不衔接冻土和融化夹层,多年冻土分布下界上升50~70m。冻土退化已对江河源寒区经济和生态环境产生了一系列重要影响。但是,冻土退缩及其对环境的影响还存在很大的不确定性。  相似文献   
162.
interpretationofpaleoclimaticrecordsinicecore(Dansgaardetal.,1969;Rozanskietal.,1997;Yao,1999;Thompsonetal.,2000).SincethefirstdeepicecorewasdrilledinGreenlandin1966(Dansgaardetal.,1969),hundredsoficecoreswereobtainedsuccessivelyfromicesheetsinAntarcticaandArctic,andmountainglaciersatmid-highlatitudes,fundedbynumerousresearchprogramsonglobalclimateandenvironmentalchange.Theseicecoresprovideuniqueandvaluablefirst-handinformationinrecoveringglobalpaleoenvironmentalrecordsandforecastingfuturecl…  相似文献   
163.
沙漠增温效应特征及绿洲农业热量资源分异规律的研究   总被引:9,自引:5,他引:9  
为了进一步认识绿洲高效农业特殊的热量资源,通过研究沙漠增温效应特征表明:沙漠增温效应强弱随距离沙漠远近而不同,100km范围内沙漠对绿洲的平均增温为1.76℃;另外增温效应导致绿洲日、年温差大、干热风及冷害等气候特征;由于沙漠的面积、地貌特点等的差异,使增温效应产生原因及作用程度不尽相同,表现出绿洲农业资源分异规律,并将西北干旱区绿洲分为5个类型区。  相似文献   
164.
信息时代地图技术美的研究与实践   总被引:3,自引:1,他引:3  
通过分析现代地图表现形式及存在的问题,探讨了信息时代地图制图技术美的含义和地图技术美的表现形式。并在技术美创新理念指导下,对利用计算机技术和图形图像处理技术来改进地图符号设计,提高地图表现力进行了一些理论探讨和技术尝试.同时也得到了一些有益的启示。  相似文献   
165.
在信息传播媒体的竞争日益严酷的时代,面对天气预报节目只依靠简单的画面加解说,拉洋片式传统方法这样一种一成不变的局面,策划创意制作出《天气资讯》节目,打破天气预报节目以往的节目形式和播出形式,以极少的投入获得最大的社会效益和经济效益。  相似文献   
166.
1. IntroductionThe basic role of urban-rural boundary layer re-search is to study all kinds of physical process changesin the atmosphere boundary layer over urban and itssurrounding areas. Urban heat island (UHI) is a well-known feature of urban-rural climate. Attempts toincrease the understanding of the causes of the UHIand other urban-rural boundary layer phenomena haveused observational, theoretical and modelling methodssince long before. Seaman (1989) used a hydrostaticmodel, with real …  相似文献   
167.
Lasafam  Iturrizaga 《Island Arc》2005,14(4):389-399
Abstract   Since the mid-nineteenth century, devastating glacier lake outbursts have occurred in the Karambar Valley. The exact source areas of these floods are to date unknown. The present study uses geomorphologic field evidence and interviews of local inhabitants to reconstruct nine potential glacier dams in the Karambar Valley within a horizontal distance of only 40 km. The article focuses on the geomorphologic reconstruction of the highest glacier dams, the Chateboi and Saklei Shuyinj Glaciers. Their lake basins were connected in former times resulting in a complex interfingering of lake sediments, lake terraces and glacial deposits. The outbursts of these lakes could have triggered the drainage of one of the lower ice-dammed lakes (Sokther Rabot, Chillinji, Warghut or Karambar) and therefore initiated an outburst cascade in the upper Karambar Valley. Successive glacier dams are wide spread in the Karakoram, and cascading lakes might have also played a role in other lake outburst scenarios. In the Karambar Valley, even today the Chateboi Glacier blocks the Karambar River over a distance of 4 km and represents a permanent hazard for the villages located downstream.  相似文献   
168.
A new efficient method is developed for the analysis of pile-group effects on the seismic stiffness and strength design of buildings with pile foundations. An efficient continuum model consisting of a dynamic Winkler-type soil element and a pile is used to express the dynamic behavior of the structure-pile-soil system with only a small numerical error. The pile-group effect is taken into account through the influence coefficients among piles which are defined for interstory drifts and pile-head bending moments. It is shown that, while the pile-group effect reduces the interstory drift of buildings in general, it may increase the bending moment of piles at the head. This means that the treatment without the pile-group effect results in the conservative design for super-structures and requires a revised member design for piles.  相似文献   
169.
Changes in the spatial scale of Beijing UHI and urban development   总被引:2,自引:1,他引:2  
The seasonal and interannual variations of Beijing urban heat island (UHI) are investigated in this paper using the temperature data from 1960 to 2000 at 20 meteorological stations in the Beijing region, and then the relationship between the intensity and spatial scale of UHI and Beijing urbanization indices is analyzed and discussed. Main conclusions are the followings. First, Beijing UHI shows obvious seasonal variations, and it is strongest in winter, next in spring and autumn, and least in summer. The seasonal variation of the UHI mainly occurs in the urban area. The UHI intensity at the center of Beijing is more than 0.8℃ in winter, and only 0.5℃ in summer. Second, the intensity of Beijing HUI exhibits a clear interannual warming trend with its mean growth rate (MGR) being 0.3088℃/10 a. The MGR of HUI is largest in winter, next in spring and autumn, and least in summer, and the urban temperature increase makes a major contribution to the growth of HUI intensity. Third, since the Reform and Opening, the urbanization indices have grown several ten times or even one hundred times, the intensity of HUI has increased dramatically, and its spatial scale also expanded distinctively along with the expansion of urban architectural complexes. Fourth, the interannual variation of urbanization indices is very similar with that of HUI intensity, and their linear correlation coefficients are significant at a more than 0.001 confidence level.  相似文献   
170.
The purpose of this study is to apply time series analysis to investigate whether the groundwater quality in the coastal area is affected by the tide. Continuous and regular in situ monitoring data of electrical conductivity (EC) and groundwater level, and tidal level data measured by the National Oceanographic Research Institute were used for the time series analysis. Through the time series analysis, it is known that EC and groundwater level conspicuously fluctuate with two periodicities (15.4 and 0.52-day), which is very similar to those of the tide. Also the behaviors of their fluctuations vary in accordance with the tidal period. These indicate that the groundwater quality has been mainly controlled by the tidal level, and the strength of tidal effect on the groundwater quality is different according to the tidal period.  相似文献   
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