The setting sun's rim flashes green, seemingly in those spots where it starts to be obscured by cloud tops.
A 30s sequence of a rare and poorly understood effect imaged by Jesper Grønne (The Art of Nature) from the Baltic Sea island of Bornholm, Denmark.
Images ©Jesper Grønne, shown with permission.
|Right: Severe enhancement of the cloud-top flash sequence shows possible hints of blue flashes.|
|The classical green flash is at the horizon as the very last sliver of sun disappears. It is the result of the sun’s rays being refracted across a layer of air warmed by the sea and is an inferior mirage. Mirage conditions of some sort – strong temperature gradients between air layers – are essential for a flash to be seen.
Another type of green flash is the mock-mirage flash. These are small, multiple and transient flashes on the sun's upper limb when the disk is still partially above the horizon. They are produced by refraction across temperature inversion layers, kinks in the normal atmospheric vertical temperature gradient where there is a layer of warmer air.
Left: 19 minutes before the cloud-top sequence above the sun passed behind another cloud bank to emerge later from its base. The upper limb shows perhaps a green limb or weak flashes indicative of another inversion layer.