首页> 外文期刊>Radio Science >First simultaneous measurement of vertical air velocity, particle fall velocity, and hydrometeor sphericity in stratiform precipitation: Results from 47 MHz wind-profiling radar and 532 nm polarization lidar observations
【24h】

First simultaneous measurement of vertical air velocity, particle fall velocity, and hydrometeor sphericity in stratiform precipitation: Results from 47 MHz wind-profiling radar and 532 nm polarization lidar observations

机译:首次同时测量层状降水中的垂直空气速度,粒子坠落速度和水凝球的球形度:47 MHz的风廓线雷达和532 nm的偏振激光雷达观测结果

获取原文
获取原文并翻译 | 示例
       

摘要

Results from simultaneous measurements of vertical air velocity (W), particle fall velocity, and hydrometeor sphericity in stratiform precipitation are reported for the first time. Cases of stratiform precipitation on 8 (case A) and 16 December 2008 (case B) observed at Sumatra, Indonesia (0.2°S, 100.32°E), are described. A 47 MHz wind-profiling radar measured W and reflectivity-weighted particle fall velocity relative to the air (VZ) simultaneously. Upward W above ∼6.0 km altitude in case B (>0.2 m s) was greater than in case A (<0.1 m s). VZ at 300 m above the 0°C altitude in case B (1.8 m s) was greater than in case A (1.3 m s). The thickness of melting layer (ML) in case B (900 m) was greater than in case A (300 m). Because the large-sized aggregates contribute to produce greater VZ and thicker ML, it is likely that entangled growth of dendritic crystals under the presence of significant upward W and enhanced aggregation occurrence by the well-developed dendritic crystals produced the large-sized aggregates. Lidar measured an increase of linear depolarization ratio (δ) and lidar dark band in the ML. Volume δ of raindrops was 0.08–0.10 in case B and close to zero in case A. Stronger multiple scattering in case B is likely a cause that produced the greater δ. In case B, a dip of δ was measured at the bottom of ML. The decrease of hydrometeor nonsphericity at the final stage of melting explains the dip.
机译:首次报告了同时测量垂直气流速度(W),颗粒下落速度和层状降水中水流星度的结果。描述了在印度尼西亚苏门答腊(0.2°S,100.32°E)观察到的8月(案例A)和2008年12月16日(案例B)的层状降水案例。一台47 MHz的风廓线雷达同时测量了W和相对于空气(VZ)的反射率加权粒子下降速度。在情况B(> 0.2 m s)中,海拔高于〜6.0 km的向上W大于情况A(<0.1 m s)。情况B(1.8 m s)高于0°C高度300 m时的VZ大于情况A(1.3 m s)。情况B(900 m)的熔化层(ML)的厚度大于情况A(300 m)的熔化层的厚度。因为大型聚集体有助于产生更大的VZ和更厚的ML,所以在显着向上的W的存在下,树枝状晶体的纠缠生长很可能,而发达的树枝状晶体增强的聚集发生则产生了大型聚集体。激光雷达测量了ML中线性去极化率(δ)和激光雷达暗带的增加。在情况B中,雨滴的体积δ为0.08-0.10,在情况A中接近零。在情况B中,较强的多次散射很可能是产生较大δ的原因。在情况B中,在ML的底部测量了δ的下降。融化最后阶段水凝液非球形性的降低解释了下降。

著录项

  • 来源
    《Radio Science》 |2012年第3期|1-14|共14页
  • 作者单位

    Research Institute for Sustainable Humanosphere, Kyoto University, Kyoto, Japan.;

    Research Institute for Sustainable Humanosphere, Kyoto University, Kyoto, Japan.;

    Faculty of System Design, Tokyo Metropolitan University, Tokyo, Japan.;

    Faculty of System Design, Tokyo Metropolitan University, Tokyo, Japan.;

    Research Institute for Sustainable Humanosphere, Kyoto University, Kyoto, Japan.;

    Graduate School of Science, Kyoto University, Kyoto, Japan.;

    Interdisciplinary Faculty of Science and Engineering, Shimane University, Matsue, Japan.;

    Faculty of Information and Communication Engineering, Osaka Electro-Communication University, Neyagawa, Japan.;

    Research Institute for Sustainable Humanosphere, Kyoto University, Kyoto, Japan.;

    Japan Agency for Marine-Earth Science and Technology, Yokosuka, Japan., SATREPS-MCCOE Promotion Office, NEONET, BPP Teknologi, Jakarta, Indonesia., Graduate School of Science, Kobe University, Kobe, Japan.;

    Research Institute for Sustainable Humanosphere, Kyoto University, Kyoto, Japan.;

    National Institute of Aeronautics and Space (LAPAN), Bandung, Indonesia.;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Atmospheric measurements; Laser radar; Radar measurements; Velocity measurement; Particle measurements; Ear;

    机译:大气测量;激光雷达;雷达测量;速度测量;颗粒测量;耳朵;
  • 入库时间 2022-08-18 00:01:00

相似文献

  • 外文文献
  • 中文文献
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号