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anomalous scattering的中文,翻译,解释,例句

anomalous scattering

anomalous scattering的基本解释
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[计] 异常散射

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Drift electron mobility, the Hall factor and Hall mobility in GaN are calculated according to Mattiessen's rule as a function of temperature for carrier concentrations with the compensation ration as a parameter on the basis of taking into account the individual average scattering momentum relaxation time of four scattering mechanisms, namely, ionized impurity scattering, polar mode optical scattering, acoustic piezoelectric scattering and acoustic phonon deformation potential scattering which have an effect on electron mobility of GaN.

考虑了对纤锌矿型氮化镓低场电子输运影响最为显著的4种散射机制-电离杂质散射,极化光学波散射,声学波压电散射和声学声子形变势散射的单个平均动量驰豫时间,采用Mattiessen's rule计算了不同补偿率以及不同载流子浓度条件下,氮化镓电子漂移迁移率,霍耳因子以及霍耳迁移率随温度的变化。

Corresponding to the long-lasting El Nio event, cyclonic anomalous circulation over the eastern North Pacific weakens slowly and anticyclonic anomalous circulation over the western North Pacific strengthens slowly at 850 hPa. Therefore the tropical Pacific westerly anomaly keeps long. The anomalous positive velocity potential over the western South Pacific at 200 hPa, which is related to the strong Australian winter monsoon, helps a long duration of El Nio. Corresponding to the short-lasting El Nio, the anomalous positive velocity potential over the western Pacific at 200 hPa moves eastward quickly and results in the vanishing of El Nio event.

还发现对于持续时间较长的El Nio事件,东北太平洋上850hPa异常气旋性环流减弱和西北太平洋上异常反气旋性环流增强较慢,因此赤道太平洋异常西风维持的时间也较长,而与澳大利亚冬季风加强相关联的南半球西太平洋的速度势正距平的维持,对El Nio的持续也起一定作用;对应持续时间较短的El Nio事件,西太平洋上200hPa速度势正距平的迅速东移,对El Nio的迅速消亡起重要作用。

Based on the Lorentz-Mie theory, the single scattering characteristics of multi-dispersed spherical and multi-layered spherical particles are studied. The extinction coefficients, scattering coefficients, single albedos, single scattering phase functions and asymmetry factors of different clouds are presented. Numerical results for single scattering of spherical and non-spherical particles are obtained in the approximation of geometrical optics. The single scattering phase matrixes of non-spherical aerosols are calculated by using the T matrix method.

基于洛伦茨-米理论研究了服从一定尺寸分布的球形和多层球形粒子的单次散射特性,计算了各种不同类型云层的消光系数、散射系数、单次散射反照率、单次散射相函数以及不对称因子;利用几何光学方法计算了球形、非球形粒子的单次散射特性;利用T矩阵方法计算了非球形气溶胶的单次散射相矩阵。

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anomalous scattering:反常散射

anomalous refraction 反常(大气)折射 | anomalous scattering 反常散射 | Anomalous Skin Effect 反常趋肤效应

anomalous scattering:異常散射= 反常散射

anomalous magnetic moment 異常磁矩= 反常磁矩 | anomalous scattering 異常散射= 反常散射 | anomalous skin effect 異常皮膚效應 = 反常趨膚效應

anomalous scattering:异常散射

"异常共振[态]","anomalous resonance" | "异常散射","anomalous scattering" | "异常肌肤效应","anomalous skin effect"

alpha anomalous scattering:粒子反常散射

铝镍钴[合金] alnico | α粒子反常散射 alpha anomalous scattering | α捕获 alpha capture

scattering, anomalous:不规则散射

散射波通讯 scattering wave communication | 不规则散射 scattering, anomalous | 反史扥克斯散射 scattering, anti-Stokes

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