瑞利 散射是指光被远小于其波长的粒子发生弹性散射的现象。这种现象造就了白天天空的蓝色。与波长较长的红色光相比,波长较短的蓝色阳光更容易被大气中的氮分子和氧分子散射,从而使天空从观察者的角度来看呈现蓝色。

(图片仅供参考)
瑞利 散射是指光被远小于其波长的粒子发生弹性散射的现象。这种现象造就了白天天空的蓝色。与波长较长的红色光相比,波长较短的蓝色阳光更容易被大气中的氮分子和氧分子散射,从而使天空从观察者的角度来看呈现蓝色。
The intensity of 瑞利 scattering is strongly dependent on the wavelength of the light, following an inverse fourth-power law: [latex]I \\propto \\lambda^{-4}[/latex]. This means that blue light (with a shorter wavelength, ~475 nm) is scattered about 16 times more intensely than red light (~700 nm) by the gas molecules in the atmosphere. When we look at the sky away from the direct sun, our eyes perceive this scattered blue light coming from all directions. Conversely, when the sun is near the horizon at sunrise or sunset, its light must travel through a much longer path in the atmosphere to reach the observer. By the time it does, most of the blue and green light has been scattered away from the direct line of sight, leaving the longer-wavelength oranges and reds to be seen. This same principle explains why distant clouds or mountains can appear bluish. Rayleigh scattering is distinct from Mie scattering, which is caused by particles of a size comparable to or larger than the wavelength of light (like water droplets in clouds) and is not strongly wavelength-dependent, which is why clouds appear white.
瑞利散射和蓝天
(如果日期未知或不相关,例如“流体力学”,则提供其显著出现的近似估计)
只有注册会员才能免费获得 100% 的全尺寸图片和下载。.
> 登录 <