新疆北天山地区中强震前单台地震波参数异常特征研究     

杨欣  曲延军 《内陆地震》1999,13(3):221-232

强地震的孕育过程也是孕震介质的形成过程,在强震前震源附近小地震的地震波运动学,动力学特征的变化过程,则反映了孕震介质的变化过程,为研究地震的孕育,发展和发生的过程,采用单台地震波振幅比,尾波持续时间比,尾波衰减系数这３项地震波参数作为地震学短期前兆指标,分析其震兆特征,从而达到监测孕震介质变化的目的,研究结果表明,单台地震波参数能够有效地发现地震的前兆,但地震波参数的前兆图像复杂多变,不具有统一的  相似文献   

ANALYSIS OF LOCATION CONDITIONS OF FINANCIAL CENTRES IN CHINA     

叶立梅  程志刚 《中国地理科学(英文版)》1993,3(4):297-307

First of all, the necessity of establishing financial centres is expounded. The establishment of financial centres has a lot of benefits to the world economic development, China's economy and the occupied cities. The location conditions of financial centres may be summarized as follows: the location of trade centre, the factors of geographical position, the circumstances of finance, etc.. We consider that the first batch of financial centres in China should be established in the eastern cities of China. So 9 eastern cities in China are chosen as the spare financial centres. According to the location conditions of financial centres, 12 indices are chosen and the method of synthetic weighted average is used to find the best locations of financial centres. The conclusions are that the grade A financial centres should be in Shanghai and the grade B should be in Tianjin and Guangzhou.  相似文献   

Experimental investigation of drag coefficients of gobi surfaces     

董治宝  屈建军  刘小平  张伟民  王训明 《中国科学D辑(英文版)》2002,45(7):609-615

The response of gobi surfaces to the near-surface air flow can be characterized quantitatively by drag coefficients. By using wind tunnel tests, an attempt is made to define the relationship between the drag coefficients of gobi surfaces and gravel size and coverage. It is concluded that the drag coefficients of gobi surfaces tend to be constants when gravel coverage is over 40%-50%. Consequently, we think that the gobi deflation planes expanding vastly in the arid Northwestern China are aerodynamically stable, at least not the supplying sources of current dust storms, and therefore the emphasis on dust storm control should be paid on the so-called "earth gobi" that has low gravel coverage. The prediction model for drag coefficients of gobi surfaces has been developed by regressing drag coefficients on gravel size and coverage, the predicted results are in reasonably good agreement with wind tunnel results (R 2 = 0.94). The change of drag coefficients with gravel friction Reynolds number implies that the development extent of drag effect increases with gravel size and coverage.  相似文献   

安徽暴雨落区与一些物理量关系的统计分析   总被引：5，自引：0，他引：5  

任敏  陈焱  璩英 《气象》2006,32(4):40-44

从概率统计的思路出发，用1994-2003年的降水资料对安徽省夏半年（4—9月）暴雨落区、频数等与5840gpm线的关系进行了统计分析，并用2003年淮河洪涝期间20个暴雨区域与某些实况物理量场对比，分析了暴雨落区与一些物理量分布的关系，表明了安徽省暴雨主要集中在梅雨期到7月份，暴雨日数多寡和暴雨范围大小，基本上主导汛期降水多少和旱涝趋势。暴雨落区集中出现在5820～5840gpm的区域，而〈5750gpm和〉5870gpm的区域很少出现暴雨。因此梅雨期主雨带位置预报大致可以用5840gpm线的移动作参考。在物理量上，西风急流北侧以及500hPa上升运动中心南侧到850hPa上升运动中心北侧，有利于暴雨发生发展。  相似文献   

基于DVB-S数据共享平台的NOAA/ATOVS资料获取、处理与显示系统          下载免费PDF全文

冉茂农  瞿建华  沙利  袁晚平  张凤英  吴雪宝 《应用气象学报》2006,17(4):502-507,i0002

充分利用国家科技部大力推行的DVB-S共享数据平台,加强气象卫星遥感数据的广泛应用,特别是发挥卫星垂直探测器(ATOVS)资料在我国数值天气预报以及监测重大灾害性天气系统中的作用。该文介绍了基于DVB-S系统的NOAA/ATOVS资料的处理、分析与显示系统的概况及主要功能,并以2005年7月人们关注的台风“海棠”为个例,展示了利用该系统在监测和分析台风或强对流天气时的独特优势。该系统的建立,将解决省、地气象部门不能实时获取ATOVS资料的问题,并将推动ATOVS资料在气象以及相关部门的实际应用。  相似文献   

2003年淮河流域致洪暴雨的环流演变   总被引：2，自引：6，他引：2  

陈晓红  冯皖平  璩瑛 《气象科学》2006,26(2):192-196

使用EC模式的格点高度场和风场资料,分析2003年6~7月欧亚地区环流形势演变特征与安徽淮河流域致洪暴雨的关系发现:淮河流域的强降雨能持续14 d之久,是500 hPa高空超长波维持2波、长波交替出现5~6波、高纬度为阻塞环流形势以及副热带高压脊长时间稳定在23~27°N偏北位置诸因子共同作用的结果。  相似文献   

The performance of the new tropical cyclone track prediction system of the China National Meteorological Center     

S. Ma  A. Qu  Y. Wang 《Meteorology and Atmospheric Physics》2007,97(1-4):29-39

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基于.NET与ArcIMS的地质灾害WebGIS系统设计与研究     

李明海  石丽梅 《地理空间信息》2007,5(3):86-88

通过对比分析目前WebGIS的常用开发方法和软件平台的特点,结合实际的应用需求,选择.NET和ArcIMS设计并实现了地质灾害信息系统。详细介绍了系统设计结构、开发方法、系统主要功能,通过属性数据与空间数据的有效连接实现了地质灾害数据发布及空间查询等。  相似文献   

Geochemical characteristics of crude oils from Well Zheng-1 in the Junggar Basin, Xinjiang, China     

李志明  张长江  秦建中  张渠  范明  刘文斌  张志荣 《中国地球化学学报》2007,26(2):163-169

Well Zheng-1 is located in the combined area of the central uplift and the north Tianshan piedmont depression in the Junggar Basin. Two oil-bearing beds are recognized at 4788–4797 m of the Lower Cretaceous Tugulu Formation (K1tg) and 4808.5–4812.5 m of the Lower Jurassic Sangonghe Formation (J1s). The geochemical characteristics of family composition, carbon isotopic composition, saturated hydrocarbons, sterane and terpane biomarkers and carotane of two crude oils are described in this paper. The results show that the geochemical characteristics of the two crude oils are basically similar to each other, indicating they were all derived mainly from the high mature, brine, algae-rich lake facies sediments. Oil-source correlation revealed that crude oils of the two beds were derived mainly from the source rocks of Permian and mixed by the oil derived from the source rocks of Jurassic and Triassic. This is consistent with the geological background with several sets of source rocks in the area studied.  相似文献   

Pulsatory characteristics of wind velocity in sand flow over typical underlying surfaces     

ZHANG KeCun  QU JianJun  ZU RuiPing & FANG HaiYan Key Laboratory of Desert  Desertification  Cold  Arid Regions Environmental  Engineering Research Institute  Chinese Academy of Sciences  Lanzhou  China 《中国科学D辑(英文版)》2007,50(2):247-253

Pulsatory characteristics of wind velocity in sand flow over Gobi and mobile sand surface have been investigated experimentally in the wind tunnel. The primary goal of this paper is to reveal the relation- ship between pulsatory characteristics of instantaneous wind speed in sand flow and the motion state of sand grains. For a given underlying surface, pulsation of wind velocities in sand flow on different heights has a good correlation. As the space distance among different heights increases, fluctuation of instantaneous wind speed presents a decreasing trend and its amplitude is closely related to the mo- tion state of sand grains and their transport. Pulsatory intensity increases with the indicated wind speed, but its relative value does not depend on it, only agrees with height.  相似文献