CINRAD/SB雷达接收机技术特点及故障诊断方法

介绍了CINRAD/SB雷达接收系统技术特点。根据接收机的主通道、测试通道、故障定位通道的信号流程,从监测信息、报警信息、关键点参数测量入手,总结了CINRAD/SB雷达接收系统故障诊断方法和技巧。详细介绍了利用RDA计算机的报警信息直接查找故障、通道测试法和关键点波形测试法3种诊断故障的方法,并列举了接收机主通道前端、后端以及测试通道3个不同类型的典型故障个例的分析和处理步骤。提出了接收系统维修方面的一些建议,为新一代天气雷达技术支持和保障提供借鉴。     

海滩上的新一代天气雷达系统防雷要点浅析

通过湛江新一代天气雷达系统的防雷设计与实际防护效果,总结地处海滩的雷达站防雷设计的要点．提出相关防雷设计思路。     

基于Ferry Borges理论的地震与重卡车作用下桥梁内力的组合问题

目前的AASHTO LRFD桥梁规范主要考虑重力荷载和卡车等活荷载的组合情况,而没有在概率基础上考虑地震等极端荷载的组合问题.包括LRFD在内的很多桥梁抗震规范都是主要考虑地震的作用,甚至设计时不考虑其他荷载的作用,LRFD设计指导手册中在考虑地震等极端荷载时,也只是提到在特殊情况和桥梁比较长的情况下再考虑卡车的作用,...     

一种工业CT点云数据的NURBS曲面重构算法

虽然CT技术已经发展得相当成熟,但保证检测数据重构的精度还存在较大困难.本文将工业CT图像转化为三维散乱点云数据,研究数据预处理算法;对处理后数据进行NURBS曲面插值,完成了对NURBs曲面的董构.以某工件工业CT图像为例,通过VG软件转化为点云数据,利用VC++和OpenGL编程实现数据预处理算法和NURBS曲面拟...     

四川九龙县溪谷输变电工程场地稳定性的岩体力学分析

溪谷输变电站工程场地具有较复杂的双层地质结构.岩土体拉分变形明显.场地后缘及底部岩土体的主应力和剪应力集中明显,堆积体内部岩体处于拉分松弛状态.岩土体的潜在变形模式以蠕滑-拉裂为主.在水库蓄水与地震共同作用的极限工况下.场地处于潜在不稳定状态.     

气候变化下淮河流域极端洪水情景预估

利用IPCC第4次评估公开发布的22个全球气候模式在A1B、A2和B1三种典型排放情景下的未来气温和降水预测结果,结合新安江月分布式水文模型,在对模型验证效果良好的基础上,参照集合预报方法,对未来90年(2010～2099年)气候变化下淮河流域的极端洪水进行预估。研究结果表明,从出现概率来看,淮河流域未来可能发生极端洪水年份的密集程度从大到小依次为A2情景、A1B情景、B1情景。A1B情景下,21世纪下半叶出现极端洪水的可能性增大,A2情景在2035～2065年以及2085年以后是极端洪水发生较为集中的时期。B1情景在21世纪70年代左右发生极端洪水的可能性较大。综合各种极端事件的定义方法,将极端洪水划定3个洪水量级。A2情景预估极端洪水的平均洪量在3种情景中最大,B1情景最小。3种情景未来一级极端洪水发生比例都比历史上偏大,A2情景下增加最多。二级极端洪水都较历史略有减少,三级极端洪水减少最显著。3种情景下各个量级极端洪水所占比例各不相同,A1B和A2情景二级以上极端洪水出现比例较大,B1情景下极端洪水量级多为三级,超1954年的一级极端洪水所占比例较小。     

Features of aerosol optical depth and its relation to extreme temperatures in China during 1980-2001

Based on Total Ozone Mapping Spectrometer (TOMS) monthly aerosol optical thickness (AOT) measurements in 1980–2001 a study is made of space/time patterns and difference between land and sea of AOT 0.50 μm thick over China,which are put into correlation analysis with synchronous extreme temperature indices (warm/cold day and night).Results suggest that 1) the long-term mean AOT over China is characterized by typical geography,with pronounced land-sea contrast.And AOT has significant seasonality and its seaso...     

开钻新工艺介绍及其优越性分析

介绍自升式钻井平台勘探二号在渤海某井作业中采用的一、二开合并钻进的开钻新工艺,并对新工艺与传统工艺对比分析,找出新工艺存在的优越性,以及使用新工艺的必要条件和技术要点。     

Sea Surface Temperature Extremes of Different Intensity in the China Seas During the Global Warming Acceleration and Hiatus Periods

Based on the daily OISST V2 with 0.25o horizontal resolutions, we study the variations of sea surface temperature (SST) extremes in the China Seas for different segments of the period 1982-2013. The two segments include the warming acceleration period from 1982 to 1997 and hiatus period from 1998 to 2013 when the global surface mean temperature (GSMT) was not significantly warming as expected during the past decades, or even cooling in some areas. First, we construct the regional average time series over the entire China Seas (15o–45oN, 105o–130oE) for these SST extremes. During the hiatus period, the regionally averaged 10th, 1th and 0.1th percentile of SSTs in each year decreased significantly by 0.40°C, 0.56°C and 0.58°C per decade, respectively. The regionally averaged 90th, 99th and 99.9th percentile of SSTs in each year decreased slightly or insignificantly. Our work confirmed that the regional hiatus was primarily reflected by wintertime cold extremes. Spatially, the trends of cold extremes in different intensity were non-uniformly distributed. Cold extremes in the near-shore areas are much more sensitivity to the global warming hiatus. Hot extremes trends exhibited non-significant tendency in the China Seas during the hiatus period. In word, the variations of the SST extremes in the two periods were non-uniform spatially and asymmetric seasonally. It is unexpected that the hot and cold extremes of each year in 1998–2013 were still higher than those extremes in 1982–1997. It is obvious that relative to the warming acceleration period, hot extremes are far more likely to occur in the recent hiatus as a result of a 0.3°C warmer shift in the mean temperature distribution. Moreover, hot extremes in the China Seas will be sustained or amplified with the end of warming hiatus and the continuous anthropogenic warming.     

江西暴雨气候特征及降水极值重现期分析

利用1961—2020年江西省83个国家气象观测站日雨量资料,采用线性倾向估计法、年最大值法以及耿贝尔Ι型极值分布理论,对江西年平均暴雨日数、暴雨降水量、暴雨贡献率、暴雨强度等的变化特征以及不同重现期的降水极值进行了分析.结果表明:1)江西各地年均暴雨日数呈西南向东北递增分布;大部分地区年暴雨日数呈增加趋势,并呈现西部和南部增加略慢,东部和东北部快速增加态势;尤其是江西东北地区既是暴雨高发中心,同时也是暴雨日数增长中心.2)江西各地年平均暴雨降水量和暴雨贡献率均呈东北多、西南少分布;景德镇和上饶为暴雨降水量和暴雨贡献率高值区也是增长中心;赣州北部和吉安南部为暴雨降水量和暴雨贡献率低值区,但呈现明显增长趋势.3)江西各地平均暴雨强度呈现较明显的北部大、南部小的分布特征;暴雨强度呈现西部增强、东部减弱的趋势.4)江西不同重现期的日雨量极值呈现东北大、西南小的分布,高值区主要分布在上饶、景德镇和抚州一带,低值区主要在吉安南部和赣州.