高级搜索

DSG5型和D17型国产降水现象仪测量参量差异分析

Analysis of Differences in Measurement Parameters between DSG5 and D17 Domestic Precipitation Phenomenon Instruments

  • 摘要: 本文统计了2022年7―10月宁夏六盘山区泾源县气象局布设的DSG5型降水现象仪、D17新型降水现象仪和SL3-1型翻斗式雨量计26次液态降水过程资料,首先对DSG5和D17观测稳定性及缺测情况,4种质控方法对DSG5和D17计算降水量的影响进行分析,其次研究D17在计算降水量上较DSG5及传统雨量计上的差异,最后对DSG5和D17在测量计算微物理参量上的差异进行比较,结果表明:(1) DSG5和D17缺测率较低,D17的漏报数低于DSG5,但空报数较DSG5高,经滤除下落末速度-直径经验公式±60%的奇异数据后,可有效降低DSG5和D17空报数。(2) 与SL3-1相比,基于2022年7―10月DSG5和D17计算的降水量均偏小,但D17计算的累积降水量与SL3-1累积降水量的相对偏差更小。(3) DSG5和D17计算的粒子数浓度(N)相差超过3倍,但雨强( R )、质量加权平均直径( D_m )、液态水含量( Q )和雷达反射率因子( Z )等微物理参量相差不大。(4) 相对于D17,DSG5观测到的大粒径的粒子样本较多,但 N 较少,故DSG5的 D_m 平均值更大, R Z 的平均值更小。(5) DSG5和D17观测到的粒子下落末速度较为接近,在粒径小于1.3 mm的情况下,与Atlas等(1973)给出的理论值相差不大,但随着降水粒子直径的增加,与理论值的偏差越来越大。

     

    Abstract: In this article, precipitation data retrieved from 26 liquid precipitation processes at the Jingyuan County Meteorological Observatory in Liupanshan, Ningxia from July to October 2022 are analyzed. Firstly, the observation stability and missing reporting of DSG5 and D17, the impact of four quality control methods on the measurements of precipitation in DSG5 and D17 are studied. Then, the differences between DSG5 and traditional rain gauges in calculating precipitation in D17, as well as the differences in measuring and calculating microphysical parameters between DSG5 and D17 are compared. The results are as follows. (1) The missing report rate of both DSG5 and D17 is low. The missing reporting of D17 is lower than DSG5 while the false reporting is highers. However, quality control methods by filtering out the empirical formula of falling velocity diameter singular data (over 60%), the number of false alarms in D17 can be effectively reduced. (2) Compared with the SL3-1 tipping bucket rain gauge, based on precipitation data from July to October,2022, the bias of D17 is less than SL3-1 in accumulated precipitation. (3) Except for particle number concentration (the bias is over 3 times), there is little difference in microphysical parameters inverted by the two instruments, rain intensity( R ), quality weighted average diameter ( D_m ), liquid water content and radar reflectivity factor ( Z ) . (4) Compared to D17, DSG5 observed more samples of particles with larger diameters as well as lower particle concentration. Therefore, on the average, DSG5 had a larger mean value of D_m and a smaller mean value of R and Z . (5) The falling velocities of particles obtained by DSG5 and D17 are relatively close. When the particle diameter is less than 1.3 mm, the falling velocity is close to the theoretical value given by Atlas et al (1973), however, with the increase of particle diameter, the bias gets larger as well.

     

/

返回文章
返回