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提出了一种新型非基于慢变包络近似的三维有限元束传播法.该方法相较Hadley所提出的广角束传播法,在分析光信号与光波导之间相互作用时同时考虑了载波和调制波对传输特性的影响,更具一般性且精度更高.通过与已发表的权威文献相比,在相同的计算资源下,精度提高了10%. 相似文献
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本文提出了一种波峰形状的低损耗微波负群时延微带电路，该电路主要由四条相同的微带传输线，两条相同的耦合微带线以及T形连接器组成.依据等效电路拓扑结构，基于微波电路理论推导出电路的S参数模型以及负群时延公式.利用ADS仿真软件对电路结构进行优化，并进行了实物的加工与测试.测试结果表明：在中心频率1.017 GHz时，电路的最大群时延为-2.46 ns，插入损耗为-2.1 dB以及反射损耗为-13 dB.实测结果与仿真结果以及理论模型结果具有很好的一致性. 相似文献
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冰水含量在气候以及天气变化、人工影响天气等方面的研究中具有重要影响。毫米波雷达在探测卷云时由于气流运动等因素的影响使得电磁波照射体积内粒子自身发生旋转运动,这为精确计算粒子散射截面以及利用其散射特性反演云中冰水含量造成困难。首先给出六种常见的非球形冰晶粒子模型,利用HFSS软件讨论特定尺寸下非球形粒子及其等效球形粒子的辐射方向图差异,利用矩量法（针对非球形粒子）以及洛伦兹-米理论（针对球形粒子）计算并拟合上述冰晶粒子在静止、水平旋转以及随机旋转三种取向下最大尺寸与后向散射截面之间的双指数关系式,假定卷云冰晶粒子混合模型满足B-H模型,云粒子的谱分布服从NASA在2007年实测的指数分布,计算出实际的冰水含量,讨论了三种取向下非球形粒子及等体积球粒子群的雷达反射率因子Z,将其代入常用的IWC-Z关系式,结果表明利用雷达反射率因子反演冰水含量时必须考虑高空风产生的粒子取向问题,等效球理论方法得到的冰水含量比实际值偏小,该结论对于毫米波雷达精确反演卷云的微观物理参数具有重要意义。 相似文献
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Ice water content (IWC) plays important roles in weather and climate change. Determining the IWCs of cirrus clouds with millimeter-wavelength radar can be problematic due to influences of ice particle rotation on their backscattering cross sections. We here introduce models to describe the radiation patterns of six nonspherical particles of specific sizes. Simulations using HFSS software were applied to describe the differences resulting from different orientations and equivalent spheres. A double exponential function was used for fitting to describe the relationship between the particles’ maximum sizes and backscattering cross sections. The backscattering cross sections of nonspherical ice particles were computed by the method of moment, and those of the equivalent spherical particles were computed by Lorenz-Mie theory for three different orientations: fixed, horizontal, and random. Assuming that a mixture of nonspherical ice particles follows the B-H mixing model, the size distribution of cirrus particles obeys the exponential distribution measured by NASA in 2007. By computing the IWCs of cirrus clouds, which follows the above mentioned B-H model and exponential distribution, the radar reflectivity factors of nonspherical ice particles and equivalent spheres at three different orientations can be computed. Subsequently, the IWC results can be acquired by inputting the radar reflectivity variables into the well-known IWC-Z formula. The analysis described here demonstrates that when using the radar reflectivity Z, the orientation must be considered in order to determine the IWC. Using equivalent sphere theory, the derived IWCs underestimate the actual IWCs. These results are important for accurately retrieving the microphysical parameters of cirrus clouds. 相似文献
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针对新一代天气雷达数据存在风轮机杂波污染问题，统计分析了5种雷达基数据特征量，风轮机杂波具有较高的反射率因子隆起度和水平通道信噪比隆起度以及较大的速度奇异率，其信号质量指数接近1，谱宽接近0或大于7.0 m·s-1。以特征量统计结果为基础，使用模糊逻辑算法对雷达基数据中的风轮机杂波进行特征识别，结果显示，模糊逻辑算法能有效地把风轮机杂波从各种强度的气象降水回波和固定地物杂波中识别出来。针对被识别出来的风轮机杂波，使用区域平均插值方法对雷达基数据中的风轮机杂波进行剔除，杂波剔除结果显示，气象降水条件下获得了较好的风轮机杂波剔除效果。 相似文献
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