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四川省闪电定位系统升级前后对比评估

Comparative evaluation of the lightning location system in Sichuan Province before and after the upgrade

  • 摘要: 针对四川省新建的78套DDW1闪电定位仪和原有19套ADTD闪电定位仪的2022年观测数据,本文对比分析了两种型号闪电定位仪及探测系统的探测性能差异。研究结果如下:1. 以海拔1000 m为界,地形显著影响闪电定位网布局:山区站间距变化大、均匀性不足,而平原则更紧凑均衡。2. DDW1和ADTD系统的地闪定位结果与雷达回波吻合度较高。3. 除甘孜站外,两系统16个同址站点的触发阈值一致性好。15个同址站点在GPS误差放大因子和噪声通过率上的一致性较高。然而,有5个同址站点存在晶振偏差值一致性的问题。4.在四川省大部分地区,DDW1系统的地闪密度约为ADTD系统的两倍,但仍然存在对四川省西部雷暴的探测能力不足的问题。ADTD探测的正、负回击电流峰值分别介于20~30 kA和-30~-20 kA;而DDW1则相应分别为10~20 kA和-20~-10 kA。DDW1的正、负回击峰值电流强度均约为相应匹配ADTD的1.04倍。5. 整体来看,同址两种设备的归一化回击电场、南北峰值磁场、东西峰值磁场和方位角的一致性较差,而回击时间和后过零点时间的一致性中等。6. DDW1和ADTD系统的地闪定位结果时间分布和子站探测的回击时间分布规律相似,均呈近似双峰分布,双峰值位于夜间,单谷值位于中午。7. ADTD子站和DDW1子站的回击捕获率均不理想。今后应研究和开发复杂地形下的传播时间修正算法和设备的计量校准技术,并应用到国家雷电观测网中。本研究成果为后续国家雷电观测网设备建设、运行和观测资料的应用等提供科学依据。

     

    Abstract: This article presents a comparative analysis of the detection performance differences between two types of lightning location systems, namely the newly built DDW1 and the original ADTD in Sichuan Province, based on the 2022 observation data of 78 DDW1 sensors and 19 ADTD sensors. The research findings are as follows: 1. Using an altitude threshold of 1000 m, topography significantly affects lightning detection network configurations: station spacing in mountainous regions varies greatly and lacks uniformity, whereas networks in plains are more compact and evenly distributed. 2. The cloud-to-ground flash positioning results of both the DDW1 and ADTD systems are found to be consistent with radar echoes. 3. With the exception of the Ganzi station, the trigger thresholds of the 16 co-located stations for both systems exhibit consistency. Furthermore, the 15 co-located stations demonstrate high consistency in terms of GPS error amplification factor and noise passing rate. However, there are 5 co-located sites that exhibit inconsistencies in crystal oscillator deviation values. 4. In most areas of Sichuan Province, the cloud-to-ground lightning density of the DDW1 system is approximately twice that of the ADTD system. However, there are still detection limitations for thunderstorms in western Sichuan Province. The positive and negative return stroke current peaks detected by the ADTD system range between 20~30 kA and -30~-20 kA respectively, while the corresponding peak values of the DDW1 system are 10~20 kA and -20~-10 kA respectively. The positive and negative return stroke peak current intensities of the DDW1 system are approximately 1.04 times that of the corresponding ADTD system. 5. Overall, the consistency of the normalized return stroke electric field, north-south peak magnetic field, east-west peak magnetic field and azimuth angle of the DDW1 and ADTD sensors at the same site is poor, while the consistency of the return stroke time and post-zero-crossing time is moderate. 6. The time distribution of cloud-to-ground flash positioning results for both the DDW1 and ADTD systems follows a similar pattern to the time distribution of return strokes detected by stations. They exhibit an approximate bimodal distribution, with peak activity observed during nighttime and a decrease during noon. 7. The capture rates of return strokes for both DDW1 and ADTD stations are found to be suboptimal. In the future, it is recommended to develop propagation time correction algorithms suitable for complex terrains and apply equipment measurement calibration technology to the National Lightning Detection Network (CNLDN). The research findings serve as a scientific basis for the subsequent construction, operation and application of CNLDN’s observation data.

     

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