Water Droplet Diffraction水滴衍射
To make the distinction between diffraction and refraction effects in the atmosphere, consider what size droplet would be necessary to produce diffraction at 22° to coincide with the 22° halo. The calculation illustrated below models the diffraction with the presumption that a small drop of water would diffract like a circular aperture. The green wavelength 500nm was chosen to model diffraction, and the circular aperture calculation was used to obtain the droplet size 2.18 microns to put the first maximum outside the central peak at 22° . 为区分大气中衍射和折射效应,考虑什么大小的水滴才能使在22°处产生的衍射效应与22°的晕相吻合。下面的计算假设一个小水滴像圆形孔径一样产生衍射。选择绿色波长500nm来模拟衍射,利用圆形孔径计算得到水滴大小为2.18微米,使第一主极大在22°处位于中央峰之外。
![]() While very small, the particle size to produce a maximum at 22° is conceivable, but the effect would be quite different from the 22° halo. The colors of the visible spectrum would be spread from about 18 to 30 degrees. The normal corona around the Sun is more like 10°, corresponding to a particle size on the order of 6 micrometers. 尽管很小,产生22°最大值的粒子尺寸是可能的,但其效果与22°晕不同。可见光谱的颜色会从大约18度到30度分布。太阳周围的正常电晕大约为10°,对应粒子尺寸约为6微米。
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Index Atmospheric optics concepts 索引:大气光学概念 | ||
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