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1.
O436.2 2006031898冰水混合云对可见光的吸收和散射特性=Absorption andscattering of light by ice-water mixed clouds[刊,中]/孙贤明(西安电子科技大学应用物理系.陕西,西安(710071)) ,韩一平∥物理学报.—2006 ,55(2) .—682-687根据Mie理论,分别计算了由纯水、纯冰和冰-水同心球形粒子构成的云层在可见光波段的单次散射特性。根据辐射传输理论,利用叠加法数值计算了这三种不同构成的云层的反射函数,以及它们的平面反照率、透过率和吸收率。结果表明,冰云和冰-水云的反射函数和平面反照率在大部分散射角下要略小于水云,而透过率却比水…  相似文献   

2.
王海华  孙贤明 《物理学报》2012,61(15):154204-154204
一种颗粒与其他种类的颗粒混合后, 会使其散射特性发生变化, 本文研究了水云中混有黑炭气溶胶后的散射特性变化. 根据Mie理论计算了水云和黑炭气溶胶散射相函数、单次散射反照率和不对称因子. 给出了混合颗粒系的蒙特卡罗模拟方法, 给出了颗粒碰撞类型抽样、自由程抽样和根据Mie相函数进行散射方向抽样的方法. 计算了光垂直入射时, 水云和黑炭气溶胶混合颗粒系的反射光强随观测角的变化, 并计算了平面反照率随入射角的变化, 讨论了黑炭气溶胶的有效半径、混合比例对整个混合颗粒系散射特性的影响. 计算结果表明, 水云中混合黑炭会加强其吸收, 且黑炭的比例和尺寸不同其散射特性差异较大.  相似文献   

3.
当云层的温度在-40℃~0℃之间时, 云层中会存在冰和水两种相态的云滴, 其散射特性与纯水云以及纯冰云特性有较大差异, 因此遥感反演混合相云层的微观和宏观物理特性具有重要的意义。本文采用冰水双层球模型模拟了冰水混合云中的云滴, 利用Mie理论计算了纯水、纯冰和冰水颗粒的单次散射特性, 分析了单次散射相函数, 不对称因子, 单次散射反照率等随着有效半径、相态、内外半径比等的变化特性。利用离散纵标法(DISORT)计算了水云和冰云对0.75 μm、2.16 μm和3.3 μm的双向反射函数, 讨论了利用纯水滴和纯冰滴反演冰水混合云滴的误差。分析结果表明, 利用0.75 μm和2.16 μm的太阳光反演冰水混合云的光学厚度和有效半径时, 光学厚度误差较大, 有效半径误差较小; 结合0.75 μm和3.3 μm的太阳光反演冰水混合云的光学厚度和有效半径时, 光学厚度误差较小, 有效半径误差较大, 其会高估其有效半径; 另外结合0.75 μm和3.3 μm这两个波长的反射函数反演冰水云的冰水混合比更为有效。  相似文献   

4.
用射线光学理论计算了具有一定尺度分布的六角冰晶粒子在可见和近红外光谱区一系列波长上(0.2~5μm)的单次散射特性.利用米氏(Mie)理论,计算了与六角冰晶具有相同截面积的球形粒子的单次散射特性.根据辐射传输理论,应用累加法,分别计算了由冰晶粒子和等效球形粒子构成的卷层云的多次散射特性,计算结果表明当入射波长λ≈3.0 μm时,等效球Mie理论可以很好地用于计算卷层云的反射特性,但是当λ<2.8μm时,尤其在可见光区,将引起显著的误差.最后提出了计算冰云光学特性的两种方案.  相似文献   

5.
基于Mie散射理论和方法,研究了航天器尾喷焰等离子体中Al2O3粒子的光学散射特性,分析了复折射率对单个Al2O3粒子消光效率因子、散射效率因子、吸收效率因子、散射相函数以及单次反照率的影响。同时,基于多分散系粒子尺度单峰分布,分析了Al2O3粒子按粒径分布后散射场的有关效应因子及散射相函数的变化,并进行了相应的数值模拟。理论和数值模拟研究表明,航天器尾喷焰等离子体Al2O3粒子复折射率的虚部和实部、粒径的大小与分布对其散射相函数、消光和散射效率因子以及单次反照率均有明显的影响。  相似文献   

6.
基于分层传输模型和Mie散射理论,在粒子散射模型中充分考虑了谱分布特征,数值模拟了800 nm飞秒激光在冰云、水云、雾、气溶胶和降雨环境中的传输特性.结果表明,谱分布和粒子相态对光丝传输特性有较大的影响.雨滴的粒径较大,光丝在降雨环境中传输时,由于散射导致的能量衰减最强,产生的光丝峰值光强和能量最低.同时,光丝能量在空间的分布不均,产生了明显的多丝结构,并导致光丝长度缩短.水云和雾具有类似的谱分布特征,光丝在水云和雾中的传输特性十分相似.但由于雾中的粒子尺度更小,光丝的能量较高,光丝分布更集中.气溶胶对光丝的散射最弱,因此在传输前期没有对光丝的结构产生影响,并以稳定的单丝结构传输,光丝的峰值光强和能量最高,但在距离成丝位置一段距离后光丝结构才逐渐出现扰动.相同谱分布下,由于冰粒子的散射能力强于水粒子,造成光丝在冰云中的能量更低,光丝分布不集中,光丝的数量明显增多.  相似文献   

7.
利用Mie理论研究了单分散煤粉颗粒对光波的散射特性,给出了单次散射相函数、消光效率因子、散射效率因子、不对称因子和单次散射反照率随粒子尺寸的变化关系;当煤粉浓度较大时,需要考虑颗粒系的多次散射特性,根据辐射传输理论,利用蒙特卡洛方法研究了煤粉颗粒的多次散射特性,并给出了其后向散射随观测角度、粒子半径和光学厚度的变化关系,计算结果对煤粉颗粒反演具有一定指导意义。  相似文献   

8.
高空卷云主要由各种不同形状的冰晶粒子组成,是地空链路上激光信号传输的重要影响因素。依据高空卷云中冰晶粒子的分布特征和散射特性,采用C版本的离散纵标法(CDISORT),充分考虑地球球形曲率及云层冰晶粒子多次散射影响因素,研究准球形边界云层的激光透过率和衰减特性,并比较了太阳天顶角不同时平面平行模式和准球面模式下卷云大气激光透过率的差异,数值计算了三种激光波长(0.65,1.06和3.8 μm)在卷云中传输时的衰减和透过特性。计算结果表明:较小太阳天顶角(小于80°)入射时,两种模式下卷云大气激光透过率相对误差很小,其中0.65 μm激光波长入射时两种模式下的相对误差仅为1.72%,较大太阳天顶角(大于80°)入射时,两种模式下卷云大气激光透过率相对误差明显增大,0.65 μm激光波长入射时两种模式下的相对误差最大达到69%;卷云粒子单次散射时,激光在云层的衰减与卷云粒子有效半径、传输距离、光学厚度及激光波长等因素有关,随光学厚度的增加,云层的激光透过率减少,1.06 μm激光波长入射时透过率最大,3.8 μm激光波长入射时透过率最小;0.65和1.06 μm激光波长入射时,随云层粒子有效半径的增加激光透过率逐渐增加,而3.8 μm波长激光,随云层粒子有效半径的增加激光透过率逐渐减少,随相对方位角的增加,云层的激光透过率减少,且不同卷云传输模型对激光透过率也存在不同的影响。该研究工作将为开展地空链路星载、机载激光通信、激光雷达探测等工程系统中的激光信号云层传输特性的应用提供理论支持,同时也可进一步拓展为地空链路激光遥感、制导和预警等应用提供预先理论研究基础。  相似文献   

9.
孙贤明  韩一平  史小卫 《物理学报》2007,56(4):2098-2105
云层上端冰雪粒子的融化形成了降雨融化层,随着粒子的下落融化过程开始,因此融化层的微观特性在垂直方向上是连续变化的.建立了降雨融化层的仿真模型,应用更为切合实际的三层球形粒子代替了融化层中的粒子.根据降雨过程中雨滴的尺寸分布推导了融化层中融化粒子的尺寸分布.根据Mie理论,计算了降雨率小于12.5 mm/h时,降雨融化层对5,10,35,94 GHz电磁波的雷达反射率和特征衰减因子的垂直廓线.计算结果表明,当电磁波频率高于20 GHz时,将无法观测到“雷达亮带”,这与实验结果相符.根据辐射传输理论,应用蒙特卡罗方法计算了垂直方向微观特性连续变化的降雨融化层对不同频率电磁波的反射率,比较了两种不同尺寸分布(Gamma分布和Marshall-Palmer分布)融化层反射率的差别,这为利用高频电磁波对降雨融化层进行遥感提供了理论和数值依据. 关键词: 降雨融化层 蒙特卡罗方法 后向散射 电磁波  相似文献   

10.
孙贤明  肖赛  王海华  万隆  申晋 《物理学报》2015,64(18):184204-184204
基于辐射传输理论, 利用蒙特卡罗方法模拟了无限窄(冲击函数)准直光束入射到典型水云以及冰水双层云时的后向散射特性, 进而将得到的冲击响应与高斯光束卷积, 得到高斯光束在云层中传输的多次散射特性. 文中给出了两种波束入射时水云以及冰水双层云的反射函数随径向r和天顶角α的变化关系, 并给出了光强在云层内部的二维分布图. 计算结果表明, 高斯光束入射时, 云层反射函数的特点与无限窄准直光束入射时有较大区别. 因此在利用激光雷达进行云层探测时需要考虑激光的散斑, 文中的方法可以为此提供理论依据.  相似文献   

11.
卷云一般分布在对流层上部到平流层下部,主要由各种形状的冰晶粒子组成。卷云散射特性的研究利用了前期建立的单个冰晶粒子散射性质数据库,并且假定卷云中粒子谱分布符合Г分布,计算得出可见光波段卷云平均散射性质:消光效率因子、吸收效率因子、单次散射反照率、非对称因子与有效尺度以及波长的变化关系。其次对计算得出的变化曲线进行分析得...  相似文献   

12.
The bulk-scattering properties of dust aerosols and clouds are computed for the community radiative transfer model (CRTM) that is a flagship effort of the Joint Center for Satellite Data Assimilation (JCSDA). The delta-fit method is employed to truncate the forward peaks of the scattering phase functions and to compute the Legendre expansion coefficients for re-constructing the truncated phase function. Use of more terms in the expansion gives more accurate re-construction of the phase function, but the issue remains as to how many terms are necessary for different applications. To explore this issue further, the bidirectional reflectances associated with dust aerosols, water clouds, and ice clouds are simulated with various numbers of Legendre expansion terms. To have relative numerical errors smaller than 5%, the present analyses indicate that, in the visible spectrum, 16 Legendre polynomials should be used for dust aerosols, while 32 Legendre expansion terms should be used for both water and ice clouds. In the infrared spectrum, the brightness temperatures at the top of the atmosphere are computed by using the scattering properties of dust aerosols, water clouds and ice clouds. Although small differences of brightness temperatures compared with the counterparts computed with 4, 8, 128 expansion terms are observed at large viewing angles for each layer, it is shown that 4 terms of Legendre polynomials are sufficient in the radiative transfer computation at infrared wavelengths for practical applications.  相似文献   

13.
A geometric optics approach including surface wave contributions has been developed for homogeneous and concentrically coated spheres. In this approach, a ray-by-ray tracing program was used for efficient computation of the extinction and absorption cross sections. The present geometric-optics surface-wave (GOS) theory for light scattering by spheres considers the surface wave contribution along the edge of a particle as a perturbation term to the geometric-optics core that includes Fresnel reflection–refraction and Fraunhofer diffraction. Accuracies of the GOS approach for spheres have been assessed through comparison with the results determined from the exact Lorenz–Mie (LM) theory in terms of the extinction efficiency, single-scattering albedo, and asymmetry factor in the size–wavelength ratio domain. In this quest, we have selected a range of real and imaginary refractive indices representative of water/ice and aerosol species and demonstrated close agreement between the results computed by GOS and LM. This provides the foundation to conduct physically reliable light absorption and scattering computations based on the GOS approach for aerosol aggregates associated with internal and external mixing states employing spheres as building blocks.  相似文献   

14.
The scattering of visible light by ice crystals and dust in radiative transfer models is challenging in part due to the large amount of scattering in the forward direction. We introduce a technique that ensures numerical conservation of photons in any radiative transfer model and that quantifies the integration error associated with highly asymmetric phase functions. When applied to a successive-orders of scatter model, the technique illustrates the high accuracy obtained in numerical integration of molecular and aerosol scattering. As well, a phase function truncation and renormalization technique is applied to scattering by ice crystals with very large size parameters, between 100 and 1000, and the scaled radiative transfer equation is solved with the spherical successive-orders model, SASKTRAN. Since computations shown this work are performed in a fully spherical model atmosphere, the computed radiances are not subject to the discontinuity at the horizon that is inherent in models using a plane–parallel assumption. The methods introduced in this work are of particular interest in modeling limb radiances in the presence of thin cirrus clouds.  相似文献   

15.
This study deals with re‐entry vehicles passing through high‐altitude clouds of ice particles. The particles disturb the flow field and are erosive, thereby increasing the turbulent heat flux considerably. Measurements were performed in a blow‐down wind tunnel to analyze the effects of a particle field on the flow. The wind tunnel flow was seeded by two aerosols. The first was used for LDV flow velocity measurements. Its size was checked by the analysis of its passage through a plane shock wave. The second aerosol was made of uniform micro‐spheres of 200 μm diameter, used to simulated the water droplets. The velocity, feeding and scattering of the latter aerosol need to be accurately measured. The velocities of the flow field and of the micro‐spheres were measured simultaneously by laser velocimetry. This paper describes the instruments used to seed, ascertain and measure this flow with two aerosols.  相似文献   

16.
Several numerical and analytical solutions of the radiative transfer equation (RTE) were compared for plane albedo in a problem of solar light reflection by sea water. The study incorporated the simplest case—a semi-infinite one-dimensional plane—parallel absorbing and scattering homogeneous layer illuminated by a monodirectional light beam. Inelastic processes (such as Raman scattering and fluorescence), polarization and air-water surface refraction-reflection effects, were not considered. Algorithms were based on the invariant imbedding method and two different variants of the discrete ordinate method (DOM). Calculations were performed using parameters across all possible ranges (single-scattering albedo ω0 and refracted solar zenith angle θ1), but with a special emphasis on natural waters. All computations were made for two scattering phase functions, which included an almost isotropic Rayleigh phase function and strongly anisotropic double-peaked Fournier-Forand-Mobley phase function. Models were validated using quasi-single-scattering (QSSA) and exponential approximations, which represent the extreme cases of ω0→0 and ω0→1, respectively. All methods yielded relative differences within 1.8% for modeled natural waters. An analysis of plane albedo behavior resulted in the development of a new extended QSSA approximation, which when applied in conjunction with the extended Hapke approximation developed earlier, resulted in a maximum relative error of 2.7%. The study results demonstrated that for practical applications, the estimation of inherent optical properties from observed reflectance can best be achieved using an extended Hapke approximation.  相似文献   

17.
In this study, we model single-scattering properties of small cirrus crystals using mixtures of polydisperse, randomly oriented spheroids and cylinders with varying aspect ratios and with a refractive index representative of water ice at a wavelength of 1.88 μm. The Stokes scattering matrix elements averaged over wide shape distributions of spheroids and cylinders are compared with those computed for polydisperse surface-equivalent spheres. The shape-averaged phase function for a mixture of oblate and prolate spheroids is smooth, featureless, and nearly flat at side-scattering angles and closely resembles those typically measured for cirrus. Compared with the ensemble-averaged phase function for spheroids, that for a shape distribution of cylinders shows a relatively deeper minimum at side-scattering angles. This may indicate that light scattering from realistic cirrus crystals can be better represented by a shape mixture of ice spheroids. Interestingly, the single-scattering properties of shape-averaged oblate and prolate cylinders are very similar to those of compact cylinders with a diameter-to-length ratio of unity. The differences in the optical cross sections, single-scattering albedo, and asymmetry parameter between the spherical and the nonspherical particles studied appear to be relatively small. This may suggest that for a given optical thickness, the influence of particle shape on the radiative forcing caused by a cloud composed of small ice crystals can be negligible.  相似文献   

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