利用毫米波云雷达数据反演层云微物理参数和云内湍流耗散率
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国家自然科学基金资助项目(41475034;41475035)


A case study on the retrieval of microphysical parameters and in-cloud stratus turbulent dissipation rate by millimeter-wave cloud radar measurement
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    摘要:

    利用地基毫米波雷达进行云参数及云内湍流特性的探测和反演。根据云雷达回波的功率谱数据,反演出大气垂直运动速度和云微物理参数,得到云内湍流耗散率ε的大小和分布情况,并进一步研究和分析了云内空气垂直运动与云微物理参数、反射率因子、多普勒速度、速度谱宽变化的关系,更好地了解云的演变情况。对2016年8月8日四川稻城的一次层状云过程的探测和反演表明:1)粒子有效半径随着上升气流的增强而增大,由于碰并聚合的作用,粒子数浓度也呈现相应减小的趋势。2)云内湍流耗散率ε在云底、云顶较大,云内较小,量级在10-8~10-2 m2·s-3,多普勒速度能谱验证了假设雷达探测湍涡的尺度在惯性副区的合理性。3)随着上升气流的增强,云粒子的下沉运动相应减小,速度谱宽相应增大。

    Abstract:

    Clouds exert an important influence on the weather and precipitation.The detection of cloud microphysical parameters(particle effective radius,drop number concentration,etc.),as well as of macro-physical parameters(cloud height,cloud thickness),is essential to studying cloud physical process and cloud radiation effects.The present paper aims to perform the detection and retrieval of cloud parameters and in-cloud turbulence characteristics with a ground-based millimeter cloud radar.By applying the Doppler spectrum data,the ambient vertical air velocity and cloud microphysical parameters are solved,whereby the turbulent dissipation rate ε and its distribution are obtained.Next,the relationships of vertical air motion to cloud microphysical parameters,radar reflectivity factor,Doppler velocity and Doppler spectrum width are thoroughly studied and analyzed so as to aid in understanding the cloud evolution.Cloud radar measurements and retrievals performed on a Stratiform cloud process case at Daocheng,Sichuan on August 8,2016 reveal the following:1)The cloud particle effective radius increases as the updraft increase,and the cloud drop number concentration decreases accordingly due to the collision-coalescence process;2)The turbulent dissipation rates ε are strong the near cloud base and cloud top,and weak in the middle layer,ranging from 10-8 to 10-2 m2·s-3.The Doppler spectrum validates the hypotheses that the turbulent scale captured by cloud radar is in the inertial subrange;3)As the air updraft grows stronger,the cloud particles deposition speed is weakened,while the Doppler spectrum width is strengthened.

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黄兴友,陆琳,洪滔,梅垚,杨敏,2020.利用毫米波云雷达数据反演层云微物理参数和云内湍流耗散率[J].大气科学学报,43(5):908-916. HUANG Xingyou, LU Lin, HONG Tao, MEI Yao, YANG Min,2020. A case study on the retrieval of microphysical parameters and in-cloud stratus turbulent dissipation rate by millimeter-wave cloud radar measurement[J]. Trans Atmos Sci,43(5):908-916. DOI:10.13878/j. cnki. dqkxxb.20180203003

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  • 收稿日期:2018-02-03
  • 最后修改日期:2018-06-11
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  • 在线发布日期: 2020-11-06
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