Coronas冠状层
A circle of light quite distinct from the 22° halo can sometimes be seen around the sun or moon if there are thin clouds composed of water droplets or ice crystals of nearly uniform size. This circle is smaller, on the order of 10°, and is caused by diffraction of light by the small particles. The appearance is often that of alternating blue-green and red circles. The diffraction by a tiny opaque barrier shows the same pattern as that of an aperture of the same size and shape in an otherwise opaque screen (Babinet's principle). 当有由水滴或冰晶组成且大小几乎均匀的薄云时,有时可以在太阳或月亮周围看到一个与22°晕不同的光圈。这个光圈大约为10°,是由光对小颗粒的衍射造成的。其外观通常呈现为交替的蓝绿色和红色圆圈。光对微小不透明障碍物的衍射显示出与同样大小和形状的孔径在其他不透明屏幕上的衍射相同的图案(布abinet原理)。
![]() The moon corona image above was taken on March 19, 2005 on a night when thin clouds were moving swiftly across the sky. The colors are subtle, but you can see a blue tint to the corona close to the moon and a reddening further out. This indicates diffraction in tiny water droplets. The shorter wavelength blue light produces diffraction maxima closer to the sun. 上面的月球电晕图像是在2005年3月19日拍摄的,那天天空中迅速移动的薄云正在掠过天空。颜色比较微妙,但你可以看到靠近月亮处有一个蓝色的色调,而更远处则呈现出红色。这表明是微小的水滴产生了衍射。波长较短的蓝光在太阳附近产生了衍射极大值。
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Index Atmospheric optics concepts 索引:大气光学概念 | ||
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Glories荣光
A rainbow band around the shadow of your aircraft seen on a cloud below is an example of a glory. For more distant clouds, the plane's shadow would be smaller, but the glory would be the same angular size if the water droplets were the same size. 飞机阴影在云层下方形成的彩色环是 glory 的一个例子。对于更远的云层,飞机的阴影会更小,但若水滴大小相同,glory 的角大小保持不变。
![]() This photo of a glory was taken by Frank Starmer and is used by permission with all rights reserved to Frank. It is remarkable in that the second order diffraction is visible and a hint of third order. 这张荣耀照片是由Frank Starmer拍摄的,经Frank许可使用,保留所有权利。其特别之处在于,第二级衍射可以明显看到,第三级衍射也有所暗示。 Below are links to posted examples of glories: 以下是已发布荣耀示例的链接:
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Index Atmospheric optics concepts 索引:大气光学概念 | |||||||||||
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Glory on Close Cloud云层密实时的光辉
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Iridescent Clouds虹彩云
The corona around the sun is often hard to see because it is close to the sun and masked by the extreme brilliance of the sun. When the same diffraction effects occur in clouds some distance from the sun which are composed of tiny uniform droplets, colorful bands or "iridescence" can be seen. The example below right shows the orientation of these iridescent clouds to the Sun, which is at the edge of the building. 太阳周围的电晕往往难以看见,因为它靠近太阳,并被太阳极端的明亮所遮蔽。当同样的衍射效应发生在太阳远处的云层中,这些云层由细小均匀的水滴组成时,可以看到彩色的条带或‘虹彩’现象。下图右所示为这些虹彩云层相对于太阳的方位,太阳位于建筑物的边缘。
Below are links to posted examples of iridescent clouds: 以下是已发布的虹彩云示例链接:
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Index Atmospheric optics concepts 索引:大气光学概念 | ||||||||
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Heiligenschein赫利根施奈
The heiligenschein or "holy light" is like the glory except that it is seen as a white glow around the shadow of your head projected on fog or mist. It can also sometimes be seen around your shadow on a rough or dusty surface (in this case called the "dry heiligenschein"). The area immediately around your head's shadow may be seen as slightly brightened by "head on" incidence of light on small particles while at slightly greater distance from the head's shadow you get darkening because you begin to see the shadows of the small particles which are now being lit at a greater angle of incidence. Dew heiligenschein can be produced by retroreflection of the light focused by tiny dewdrops, while this light from droplets further from your head's shadow does not reach your eyes. ‘圣光’或‘ holy light ’是一种类似光辉的现象,但它是看到你的头影投射在雾或薄烟上的白色光芒。它有时也可以看到在粗糙或尘土表面的阴影周围(此时称为‘干圣光’)。在你头影的附近区域,由于光线直接照射到小颗粒上,可能会显得略微明亮;而在稍远于头影的位置,由于开始看到小颗粒的阴影,光线以更大的入射角照射,因此会变暗。‘露圣光’可以通过微小露珠的反光产生,而远离头影的露珠发出的光则无法到达眼睛。
Examining dew heiligenschein a bit more closely, following the discussion of Lynch and Livingston, tiny dewdrops act as essentially spherical lenses, focusing the light at a distance of about 0.7 x the drop radius behind the drop. If that concentrated light strikes a leaf or blade of grass, part of it is retroreflected through the droplet, proceeding backward toward our eyes. The retroreflection produces the appearance of a bright diffuse glow around the viewer's head. It is spread over a few degrees by the fact that the droplet "lenses" have large amount of aberration and don't send their light back at exactly 180° . 仔细观察露珠的halo现象,参照Lynch和Livingston的讨论,微小的露珠基本上像球形透镜,将光聚焦在约0.7倍露珠半径之后的点上。如果这种聚焦的光照射到叶子或草叶上,部分光会通过露珠 retroreflected 回来,朝向我们的眼睛。这种retroreflection产生了一种明亮的扩散光晕,围绕在观察者头部周围。这种光晕覆盖几个度,是因为露珠“透镜”具有较大的像差,不能将光精确地以180°方向反射回去。 Below are links to posted examples of heiligenschein: 以下是一些关于heiligenschein的示例链接:
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Index Atmospheric optics concepts Reference Lynch and Livingston Sec 4.12 索引 大气光学概念 参考 Lynch 和 Livingston 第4.12节 | ||||||||
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Specter of the Brocken布洛克鬼影
![]() Below are links to posted examples of the Specter of the Brocken: 以下是一些关于布罗克山幽灵的示例链接:
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Index Atmospheric optics concepts 索引:大气光学概念 | ||||||||
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