• 文献检索
  • 文档翻译
  • 深度研究
  • 学术资讯
  • Suppr Zotero 插件Zotero 插件
  • 邀请有礼
  • 套餐&价格
  • 历史记录
应用&插件
Suppr Zotero 插件Zotero 插件浏览器插件Mac 客户端Windows 客户端微信小程序
定价
高级版会员购买积分包购买API积分包
服务
文献检索文档翻译深度研究API 文档MCP 服务
关于我们
关于 Suppr公司介绍联系我们用户协议隐私条款
关注我们

Suppr 超能文献

核心技术专利:CN118964589B侵权必究
粤ICP备2023148730 号-1Suppr @ 2026

文献检索

告别复杂PubMed语法,用中文像聊天一样搜索,搜遍4000万医学文献。AI智能推荐,让科研检索更轻松。

立即免费搜索

文件翻译

保留排版,准确专业,支持PDF/Word/PPT等文件格式,支持 12+语言互译。

免费翻译文档

深度研究

AI帮你快速写综述,25分钟生成高质量综述,智能提取关键信息,辅助科研写作。

立即免费体验

光学厚介质中的渐近辐射度与偏振:海洋与云层。

Asymptotic radiance and polarization in optically thick media: ocean and clouds.

作者信息

Kattawar G W, Plass G N

出版信息

Appl Opt. 1976 Dec 1;15(12):3166-78. doi: 10.1364/AO.15.003166.

DOI:10.1364/AO.15.003166
PMID:20168409
Abstract

Deep in a homogeneous medium that both scatters and absorbs photons, such as a cloud, the ocean, or a thick planetary atmosphere, the radiance decreases exponentially with depth, while the angular dependence of the radiance and polarization is independent of depth. In this diffusion region, the asymptotic radiance and polarization are also independent of the incident distribution of radiation at the upper surface of the medium. An exact expression is derived for the asymptotic radiance and polarization for Rayleigh scattering. The approximate expression for the asymptotic radiance derived from the scalar theory is shown to be in error by as much as 16.4%. An exact expression is also derived for the relation between the diffusion exponent k and the single scattering albedo. A method is developed for the numerical calculation of the asymptotic radiance and polarization for any scattering matrix. Results are given for scattering from the haze L and cloud C3 distributions for a wide range of single scattering albedos. When the absorption is large, the polarization in the diffusion region approaches the values obtained for single scattered photons, while the radiance approaches the value calculated from the expression: phase function divided by (1 + kmicro), where micro is the cosine of the zenith angle. The asymptotic distribution of the radiation is of interest since it depends only on the inherent optical properties of the medium. It is, however, difficult to observe when the absorption is large because of the very low radiance values in the diffusion region.

摘要

在诸如云层、海洋或浓厚行星大气层等既散射又吸收光子的均匀介质深处,辐射亮度随深度呈指数下降,而辐射亮度和偏振的角度依赖性与深度无关。在这个扩散区域,渐近辐射亮度和偏振也与介质上表面的入射辐射分布无关。推导出了瑞利散射的渐近辐射亮度和偏振的精确表达式。结果表明,从标量理论导出的渐近辐射亮度的近似表达式误差高达16.4%。还推导出了扩散指数k与单次散射反照率之间关系的精确表达式。开发了一种用于数值计算任意散射矩阵的渐近辐射亮度和偏振的方法。给出了针对广泛的单次散射反照率,从霾L和云C3分布进行散射的结果。当吸收很大时,扩散区域内的偏振接近单次散射光子所获得的值,而辐射亮度接近由以下表达式计算得出的值:相函数除以(1 + kmicro),其中micro是天顶角的余弦。辐射的渐近分布很重要,因为它仅取决于介质的固有光学特性。然而,当吸收很大时,由于扩散区域内的辐射亮度值非常低,很难进行观测。

相似文献

1
Asymptotic radiance and polarization in optically thick media: ocean and clouds.光学厚介质中的渐近辐射度与偏振:海洋与云层。
Appl Opt. 1976 Dec 1;15(12):3166-78. doi: 10.1364/AO.15.003166.
2
Radiance and polarization of light reflected from optically thick clouds.从厚光学云层反射的光的辐射度与偏振度。
Appl Opt. 1971 Jan 1;10(1):74-80. doi: 10.1364/AO.10.000074.
3
Multiple scattered radiation emerging from Rayleigh and continental haze layers. 1: Radiance, polarization, and neutral points.来自瑞利散射层和大陆霾层的多重散射辐射。1:辐射率、偏振和中性点。
Appl Opt. 1976 Mar 1;15(3):632-47. doi: 10.1364/AO.15.000632.
4
Effect of changes in complex part of the refractive index on polarization of light scattered from haze and clouds.折射率复部变化对雾和云散射光偏振的影响。
Appl Opt. 1969 Dec 1;8(12):2489-95. doi: 10.1364/AO.8.002489.
5
Radiance and polarization of multiple scattered light from haze and clouds.来自雾霾和云层的多次散射光的辐射度与偏振
Appl Opt. 1968 Aug 1;7(8):1519-27. doi: 10.1364/AO.7.001519.
6
Matrix operator theory of radiative transfer. 2: scattering from maritime haze.辐射传输的矩阵算子理论。2:海洋薄雾散射
Appl Opt. 1973 May 1;12(5):1071-84. doi: 10.1364/AO.12.001071.
7
Influence of single scattering albedo on reflected and transmitted light from clouds.单次散射反照率对云层反射光和透射光的影响。
Appl Opt. 1968 Feb 1;7(2):361-7. doi: 10.1364/AO.7.000361.
8
Polarization of the Radiation Reflected and Transmitted by the Earth's Atmosphere.地球大气反射和透射辐射的偏振
Appl Opt. 1970 May 1;9(5):1122-30. doi: 10.1364/AO.9.001122.
9
Radiation in the earth's atmosphere: its radiance, polarization, and ellipticity.地球大气中的辐射:其辐射度、偏振和椭圆率。
Appl Opt. 1976 Oct 1;15(10):2489-500. doi: 10.1364/AO.15.002489.
10
Ocean-atmosphere interface: its influence on radiation.海洋-大气界面:其对辐射的影响。
Appl Opt. 1981 Mar 15;20(6):917-31. doi: 10.1364/AO.20.000917.