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81.
用小波变换提取雷达回波图像中的辐合特征线 总被引:1,自引:1,他引:0
采用小波变换的方法对滨州雷达资料的反射率图像进行处理,得到特征线增强后的图像,将其输入自动预报系统实现特征识别,可为雷暴预报提供初步资料。 相似文献
82.
83.
插件技术在天气雷达数据处理软件中的应用 总被引:4,自引:2,他引:4
介绍了在多普勒天气雷达二次产品软件的编写中使用动态链接库(Dynam—ic—link Library)技术设计的一个插件系统(Plug—in System)。该系统中所有的算法都设计成插件,将产品算法部分和系统本身分离,便于工程的管理和进一步开发,使研究人员能够集中精力致力于算法的实现。该系统本身也可以作为一个新算法、新产品的开发平台。 相似文献
84.
Petrogenesis and significance of early Yanshanian syenite-granite complex in eastern Nanling Range 总被引:4,自引:2,他引:4
CHEN Peirong ZHOU Xinmin ZHANG Wenlan LI Huimin FAN Chunfang SUN Tao CHEN Weifeng & ZHANG Min . State Key Laboratory of Mineral Deposits Research Department of Earth Sciences Nanjing University Nanjing China . Tianjin Institute of Geology Mineral Resources China Geological Survey Tianjin China 《中国科学D辑(英文版)》2005,48(7)
According to the statistics for granitoid distribution map of 1/2000000 Nanling region[1], the granitoids in the Nanling region sum up an area of more than 170000 km2, occupying about one fifth of the entire Nanling region. Granitoid rocks in the Nanlingregion are mainly composed of monzogranites (occu- pying more than 84%), granodiorites (about 11%) and syenogranites (about 3%)[2]. There also exists a small amount of syenites (0.12%) with a sum area of about 94 km2[2]. However, nearly half … 相似文献
85.
Disequilibria between 210Po and 210Pb in surface waters of the southern South China Sea and their implications 总被引:1,自引:0,他引:1
Yang Weifeng Huang Yipu Chen Min Zhang Lei Li Hongbin Liu Guangshan Qiu Yusheng 《中国科学D辑(英文版)》2006,49(1):103-112
Activities of the naturally occurring radionuclides, 210Pb and 210Po, were measured in both dissolved (<0.45 μm) and particulate (>0.45 μm) phases from surface waters of the southern South
China Sea. The average activity of particulate 210Pb, 0.23 Bq/m3 (n=23), accounted for about 12% of the total 210Pb, which corresponds with values of open oceans. Particulate 210Po, with an average activity of 0.43 Bq/m3, accounted for about 40% of the total 210Po, which was much higher than those of open and eutrophic oceans. The residence times of total 210Po and 210Pb in surface waters estimated from an irreversible steady-state model were 0.82 a and 1.16 a, respectively. The consistently
high fractionation factor calculated either by scavenging rate constants (5.42) or Kd values (6.69) suggested that a significant fractionation occurred between 210Po and 210Pb during their removal from solution to particles and that the two radionuclides had different biogeochemical cycling pathways
in the oligotrophic South China Sea. Furthermore, our results indicated that there exist different fractionation mechanisms
between 210Po and 210Pb in different marine environments: in eutrophic ocean, plankton detritus and fecal pellets are the main carrier of 210Po and 210Pb, by which 210Po and 210Pb have been scavenged and removed; while in oligotrophic ocean, microbes could become the main carrier of 210Po and fractionate 210Po and 210Pb significantly as a result of scarce plankton detritus and fecal pellets. These results suggest the use of 210Po to trace marine biogeochemical processes relating to microbial activities and the cycling of sulfur group elements (S,
Se, Te and Po). 相似文献
86.
Taking advantage of the actual continuous materials of hilly area, we analyse the structures of the wind and temperature fields of planetary bounday layer over hill terrain under different weather conditions. As the results show that being similar to the situation in flat area, the planetary boundary layer has striking characteristics of daily variation and distinct regularity. We also find that in certain weather situation or under certain weather condition, these characteristics are principally determined by complex effect of such factors as the features of specific radiation field and intensity of turbulent exchange, and the advection of wind, and the thermodynamic effect of valley or lake-land, and the extending direction of valley, as well as difference between states of sunlessness and sunshine of the surface. Therein, the local environmental situation, where the reference station stands, is of considerable importance to the formation of the characteristics of planetary boundary over hill terrain (shortened as HTBL). These results not only help us to disclose the characteristics of planetary boundary layer over hill terrain in theory, but also are of great value in practice, like developing hilly area, and implementing environment conservation etc. 相似文献
87.
The distribution of monthly mean error of NMC model forecasts and its seasonal variation are investi-gated.The ratio of monthly mean error to standard deviation is used here to find out that the region where acorrection of systematic error is needed and appropriate is mainly in low latitudes.The improvement,afterthe model's vertical resolution and some physical parameters were changed from April 1985,is investigated,andthe NMC operational model forecasts have also compared with those of ECMWF. 相似文献
88.
塔里木盆地西南坳陷中新统安居安组辫状河三角洲沉积 总被引:4,自引:1,他引:4
在塔里木盆地西南坳陷中新统安居安组中发现一套辫状河进积到内陆湖泊中而形成的辫状河三角洲沉积体。三角洲3层结构清楚,可明显地分为辫状河三角洲平原亚相、辫状河三角洲前缘亚相及前三角洲亚相3部分,可识别出7种微相。辫状河三角洲特征显著,明显有别于扇三角洲和曲流河三角洲。辫状河三角洲的主体是由含砾砂岩及中、粗粒砂岩组成的辫状河道砂坝及水下分流河道砂坝,单一砂坝呈下粗上细的透镜状,透镜体最大厚度为0.7~3.5m不等。垂向上许多砂坝透镜体相互叠置而成厚的砂体。三角洲中交错层理丰富,其中尤以水道砂坝侧向迁移加积而形成的侧积交错层异常发育为标志。辫状河三角洲砂体是重要的油气储集场所。 相似文献
89.
90.
Environmental change and cultural response around 4200 cal. yr BP in the Yishu River Basin, Shandong
Neolithic culture series in the Yishu River Basin developed in the order of Beixin culture–Dawenkou culture–Longshan culture–Yueshi culture. During the early and middle stage of Longshan culture (4600–4300 cal. yr BP), the climate in the Yishu River Basin was warm and wet. Paddy-oriented agriculture planted paddy was very developed. The society was flourishing with great amount of archaeological sites. The cooling starting in 4200 cal. yr BP made the paddies shortfall in output or even no seeds were gathered. This situation in-tensified the discrepancy between population and resource. The scarcity in natural resource led to substantial decrease in population and subsequent drop in archaeological sites. About 4000 cal. yr BP Longshan culture was displaced by Yueshi culture which was relatively un-derdeveloped, simple and unsophisticated. 相似文献