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太赫兹频段雷达探测的冰云微物理参数反演算法模拟研究
引用本文:丁霞,黄兴友,王海涛.太赫兹频段雷达探测的冰云微物理参数反演算法模拟研究[J].热带气象学报,2019,35(1):63-72.
作者姓名:丁霞  黄兴友  王海涛
作者单位:1.上海无线电设备研究所,上海 200090
基金项目:国家自然科学基金41475034上海市自然科学基金16ZR1434900上海市自然科学基金17ZR1428700上海市科学技术委员会工程技术研究中心建设立项15DZ2250800
摘    要:在假设冰云粒子呈球形以及粒子谱服从对数正态分布的条件下,利用离散偶极子近似法(DDA),计算出太赫兹频段(220 GHz)冰云粒子的雷达反射率因子,及其与瑞利假设下雷达反射率因子的比值。忽略衰减和多次散射的影响,根据太赫兹波段冰云的雷达反射率因子,基于最优估计理论反演冰云的微物理参数,并验证该算法的可靠性。反演结果表明,当冰云粒子大小在设定的尺度范围内时,有效粒子半径(re)的反演误差小于4%,粒子谱宽(σ)的误差小于2.5%、粒子数密度(NT)的误差小于1%,冰水含量(IWC)的误差小于5%。还分析了当NT和σ为定值时,反演结果随粒子尺寸的变化情况,当冰云粒子尺寸在模拟计算设定的范围内时,re的反演误差小于0.04%,σ的反演误差小于0.02%,NT的反演误差小于0.50%,IWC的反演误差小于0.08%,如果冰云粒子大小超出模拟计算设置的范围,反演误差随着re增加而增大。该结果证明了基于最优估计理论反演得到的冰云微物理参数与模拟设定值有良好的一致性,说明该方法可应用于太赫兹频段云雷达的冰云观测及云微物理参数的反演和研究。 

关 键 词:太赫兹    冰云    最优估计    云微物理参数    反演
收稿时间:2017-12-12

SIMULATION RESEARCH OF ICE CLOUD MICROPHYSICAL PARAMETERS RETRIEVAL WITH THZ-BAND RADAR MEASUREMENT
Institution:1.Shanghai Radio Equipment Research Institute, Shanghai 200090, China2.Shanghai Engineering Research Center of Target Identification and Environment Perception, Shanghai 200090, China3.Nanjing University of Information Science & Technology, Nanjing 210044, China
Abstract:With the assumption that ice cloud droplets are spherical and size spectra follows lognormal distribution, the factor of radar reflectivity of the ice cloud droplets and their ratio to that with the Rayleigh assumption are determined for the frequency of THz (220 GHz) by adopting the DDA (Discrete Dipole Approximation) algorithm. Without considering the attenuation and multiple scattering effects, the characteristic parameters for ice cloud particles are retrieved using the simulated radar reflectivity factor of ice clouds. Based on the optimal estimation theory the retrieval algorithm is verified to be reliable in the THz band according to the simulated radar reflectivity factor of ice clouds. The retrieval result of a case study shows that retrieval error of effective radius(re), width parameter(σ), number concentration(NT) and ice water content(IWC) are less than 4%, 2.5%, 1% and 5%, respectively, when the ice cloud particle size distribution is in the range of simulation setting. Then the retrieval variation with ice cloud particle size is analyzed with NT and σ set as constants; when the ice cloud particle size distribution is in the range of simulation setting, retrieval error of retrieved re, σ, NT and IWC is less than 0.04%, 0.02%, 0.50% and 0.08%, respectively, otherwise the retrieval error increases with re. These results have proved that retrieved ice cloud microphysical parameters are well consistent with simulated real values, so this retrieval algorithm based on optimal estimation theory can be useful for observation and retrieval research of ice cloud microphysical parameters with THz cloud profiling radars. 
Keywords:
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