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利用新疆伊犁河谷高密度地面自动站逐小时降水观测资料,对2010-2022年暖季(5-9 月)短时强降水(flash heavy rain,FHR)逐1h、3h和6h时空分布特征进行分析,结果发现:伊犁河谷暖季不同历时短时强降水阈值空间分布具有一致性,1h、3h和6h极端降水阈值的平均值分别为 8.5mm?h-1 、12.6mm?(3h)-1和16.8mm?(6h)-1。不同历时FHR集中发生在5月中旬至8月中旬,其中6月最多,7月次之;不同历时FHR频次发生在中午13:00至下午18:00。不同历时FHR事件最大小时雨强的月分布与发生站次略有差异,除1h最大为62.6mm?h-1出现在7月外,其他雨强均出现在6月分别为89.9mm?(3h)-1、104.5mm?(6h)-1,较大值位于河谷东部和南部。伊犁河谷暖季不同历时FHR空间分布具有明显的不对称性特征,总体呈东高西低的分布格局,在南北方向上1h短时强降水呈北高南低,3h、6h短时强降水均无明显变化趋势。不同历时FHR降水贡献和发生频率的局地差异明显,存在多个大值中心,主要出现在新源县、昭苏县偏北地区、霍城县偏北地区、特克斯县偏西地区、尼勒克县偏西地区及伊宁县中部等地。FHR频次各站虽有显著差异,但未发生明显离散,地形对FHR的增幅作用显著。 相似文献
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气象仪器检定管理系统设计 总被引:1,自引:0,他引:1
基于VB语言和ACCESS数据库技术构建气象仪器检定管理系统,根据气象仪器的管理特点,主要设计了仪器检定模块和主动管理模块,实现对气象仪器日常管理的信息化. 相似文献
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RTK差分技术在网约车计费系统检测中的应用 总被引:1,自引:0,他引:1
2013年以来,随着打车软件的流行,网络约车不断进入人们的视野并活跃在全国各大城市。随之而来的网络约车软件定位不准、计程不准而导致的客户投诉也接踵而来。针对这些问题,本文提出了一套网络约车计费检测方法,采用多模多频RTK载波相位差分技术和惯性导航组合定位技术,使用基准站+流动站的RTK差分GNSS接收机、惯导模块、高精度扼流圈导航天线及回放仪记录汽车行驶过程中的信息,包括经纬度、乘车时间、速度等,通过计算得出汽车行驶里程。通过与司机手机计费结果进行比较,试验结果表明,采用载波相位差分技术和组合导航定位的技术可以有效解决定位失锁、轨迹不连续等问题。 相似文献
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ZHU Xiaoqing 《中国地球化学学报》2005,24(4):306-315
Experimental studies were undertaken on leaching of sedimentary rocks ( dolomite and sandstone) and Hg, Sb ores by distilled water under the condition of a completely open system (room temperature and room pressure). The aim is to find whether the halogen elements or metal elements first enter the solution at the early stage of meteoric waters converting to groundwaters and ore fluids, and, at the same time, to understand how and when they enter distilled water solutions from the rocks. The experimental resuhs have shown that F and Cl began to enter the fluids in the initial period of thirty days. With increasing leaching duration, the amounts of the elements that entered the fluids increased steadily. During the period from 120 days to 150 days the amounts increased more drastically, followed a slow increase. It is found that the capability of Cl entering the solutions is much greater than that of F. Hg and Sb were found not to have entered the solutions till 120 days later. During this period of time the pH value of the solutions began to drop. As for Hg and Sb ores, Hg and Sb began to enter the solutions on the 60th or 90th day, greatly ahead of schedule, but the two metallic elements in the rock samples began to enter the solutions 150 days later. Relatively speaking, Hg is more easily leached out than Sb from the rocks. In some rock samples, Sb could be detected in the solutions at the end of the experiment. However, Cu, Pb and Zn had not been detected in the leaching solutions from the beginning to the end of the experiment. In the whole leaching process the pH value of the solutions tend to decrease slowly from 7.1 at the beginning to 6.5 at the end. That is to say, in the interaction between pure water and rock the halogen elements in the rocks were preferentially leached out and then entered the fluids. With increasing water/rock reaction duration and amount of halogen-group elements in the solution and with decreasing pH value of the solution, some active metallic elements began to release in small amounts. This experimental result can explain the source and mechanism of volatile components and trace metals in underground waters. Meanwhile, as for those ore deposits produced by ore fluids derived from meteoric waters, the experimental result is also helpful to the understanding of the geochemical variation trend at the initial stage of conversion of meteoric waters to ore fluids. 相似文献