Gedzelman Stanley David
Appl Opt. 2017 Jul 1;56(19):G128-G135. doi: 10.1364/AO.56.00G128.
Three scenarios that produce colored thunderstorms are simulated. In Scenario #1, the thunderstorm's sunlit face exhibits a color gradient from white or yellow at top to red at base when the sun is near the horizon. It is simulated with a second-order scattering model as a combination of sunlight and skylight reflected from the cloud face that is attenuated and reddened by Rayleigh and Mie scattering over the long optical path near sunset that increases from cloud top to base. In Scenario #2, the base of the precipitation shaft appears luminous green-blue when surrounded by a much darker arcus cloud. It is simulated as multiply scattered light transmitted through the precipitation shaft using a Monte Carlo model that includes absorption by liquid water and ice. The color occurs over a wide range of solar zenith angles with large liquid water content, but the precipitation shaft is only bright when hydrometeors are large. Attenuation of the light by Rayleigh and Mie scattering outside the precipitation shaft shifts the spectrum to green when viewed from a distance of several kilometers. In Scenario #3, the shaded cloud face exhibits a "sickly" yellow-green color. It is simulated with a second-order scattering model as the result of distant skylight that originates in the sunlit region beyond an opaque anvil of order 40 km wide but is attenuated by Rayleigh and Mie scattering in its path to the cloud and observer.
模拟了三种产生彩色雷暴的情景。在情景#1中,当太阳接近地平线时,雷暴被阳光照射的面呈现出从顶部的白色或黄色到底部的红色的颜色梯度。它是用二阶散射模型模拟的,作为从云面反射的阳光和天光的组合,在日落附近的长光程上,由于瑞利散射和米氏散射,从云顶到底部光程增加,光线被衰减并变红。在情景#2中,当降水柱底部被暗得多的弧状云包围时,会呈现出发光的蓝绿色。它是用蒙特卡罗模型模拟的,该模型将多次散射光透过降水柱,其中包括液态水和冰的吸收。这种颜色在太阳天顶角范围很广且液态水含量大的情况下都会出现,但只有当水凝物较大时,降水柱才会明亮。当从几公里外观察时,降水柱外瑞利散射和米氏散射对光的衰减会使光谱向绿色偏移。在情景#3中,被遮蔽的云面呈现出“病态”的黄绿色。它是用二阶散射模型模拟的,是远处天光的结果,这种天光起源于一个40公里宽的不透明砧状云以外的阳光照射区域,但在其到达云层和观察者的路径中被瑞利散射和米氏散射衰减。