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green flash

 
 
green flash or emerald flash, a refractive phenomenon of the atmosphere where the top edge of the setting (or, less frequently, rising) sun will momentarily turn emerald green. The green color lasts from a fraction of a second to two seconds. It is usually seen over a low distant horizon, such that as of the ocean or a prairie, when the sky is clear and free of clouds. The phenomenon was explained by James Prescott Joule in a letter to the Manchester Literary and Philosophical Society in 1869 and popularized in Jules Verne's novel Le Rayon Vert (1882; tr. The Green Ray, 1883).

The green flash occurs primarily because the atmosphere acts like a weak prism, refracting sunlight and separating it into different colors. As the sun sets, red and orange light, which are refracted the least, disappear first. Although green light is in roughly the middle of the spectrum, it is usually the last color to be seen by someone watching a sunset because blue and violet light are practically all absorbed by the contamination in the atmosphere, which scatters blue light and removes it from the line of sight. Under extraordinary conditions, however, a "blue flash" may be seen. At sunrise the phenomenon is reversed, with the green flash appearing first.


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Boating Encyclopedia: Green Flash
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Where to look for a rare atmospheric phenomenon
The legendary green flash of the sun is rarely seen, but it certainly exists. If you’re lucky you’ll see it, when atmospheric conditions are right, in the last rays of the sun as it sinks into the sea. Several well-known ocean voyagers have noted it, and I have seen it myself on a calm evening in the southeast trades.It is very short-lived, lasting only a fraction of a second to (at most) a few seconds. It is a misnomer because there is no flash—just a green glow at the top edge of the sun. You may prolong it slightly by standing up as it occurs.It’s caused by refraction of the sun’s light through the Earth’s atmosphere, which separates the light into different colors. Blue light is bent more strongly than red light and the separation is exaggerated vertically, so the blue light is the last to be seen. But contamination in the atmosphere scatters blue light and removes it from our line of sight, leaving mainly green light to be observed.According to experts at the Mount Wilson Observatory, near Los Angeles, where the green flash is frequently observed, it is also possible to see a blue flash in extraordinary conditions.You’re most likely to see the green flash in a calm and stratified atmosphere. As the sun gets closer to the horizon, it distorts and flattens in the vertical direction, and soon its edge becomes “notched” on both sides. The notches seem to be riding up the sides of the sun, but it’s actually the sun that’s moving down while they stay still.When the notches get to the top of the sun, they meet and pinch off the edge of the disk so that it looks like a floating cloud—this is the part that suddenly turns green.


Wikipedia: Green flash
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Development of Green Flash

Green flashes and green rays are optical phenomena that occur shortly after sunset or before sunrise, when a green spot is visible, usually for no more than a second or two, above the sun, or a green ray shoots up from the sunset point. Green flashes are actually a group of phenomena stemming from different causes, and some are more common than others.[1] Green flashes can be observed from any altitude (even from an aircraft). They are usually seen at an unobstructed horizon, such as over the ocean, but are possible over cloud-tops and mountain-tops as well.

A larger than usual green flash in Santa Cruz

Contents

Explanation

Stages of a green flash
Mock Mirage green flash observed in San Francisco

The reason for a green flash lies in refraction of light (as in a prism) in the atmosphere: light moves more slowly in the lower, denser air than in the thinner air above, so sunlight rays follow paths that curve slightly, in the same direction as the curvature of the Earth. Higher frequency light (green/blue) curves more than lower frequency light (red/orange), so green/blue rays from the upper limb of the setting sun remain visible after the red rays are obstructed by the curvature of the earth.

Green flashes are enhanced by mirage, which increase the density gradient in the atmosphere, and therefore increase refraction. A green flash is more likely to be seen in clear air, when more of the light from the setting sun reaches the observer without being scattered. We might expect to see a blue flash, but the blue is preferentially scattered out of our line of sight and remaining light ends up looking green.

With slight magnification a green rim on the top limb of the solar disk can be seen on most clear-day sunsets. However the flash or ray effects require a stronger layering of the atmosphere and a mirage which serves to magnify the green for a fraction of a second to a couple of seconds.

Types of green flashes

The green flash is actually a group of phenomena, some of which are listed below:[1]

Type Characteristics Conditions Best seen from...
Inferior-mirage flash Joule's "last glimpse"; oval, flattened below. Lasts 1 or 2 seconds. Surface warmer than the overlying air Close to sea level
Mock-mirage flash Indentations seem to "pinch off" a thin, pointy strip from the upper limb of the Sun. Lasts 1 or 2 seconds. Atmospheric inversion layer below eye level; surface colder than air. The higher the eye, the more likely; flash is most obvious when the eye is just above the inversion.
Sub-duct flash Large upper part of an hourglass-shaped Sun turns green for up to 15 seconds. Observer below a strong atmospheric inversion In a narrow height interval just below a duct (can occur at any height)
Green ray Green beam of light either shooting up or seen immediately after sundown. Usually few degrees long, lasting several seconds. Hazy air and a bright green flash acting as a light source Unknown

The majority of flashes observed are inferior-mirage or mock-mirage ones, with the others constituting only 1% of reports. Some types not listed in the table above, such as the cloud-top flash (seen as the sun sinks into a coastal fog, or at distant cumulus clouds), are not understood.[1]

Blue flashes

Very occasionally, the amount of blue light is sufficient to be visible as a "blue flash".[2] The term should not be confused with the similar usage of blue flash referring to the blue light seen in nuclear criticality accidents.

Green rim

Upper rim is green and lower rim is red while the sun is setting behind the Golden Gate Bridge

As an astronomical object sets or rises, the light it emits travels through the atmosphere, which works as a prism separating the light into different colors. The color of the upper limb of an astronomical object could go from blue to green to violet depending on the decrease in concentration of pollutants as they spread throughout an increasing volume of atmosphere.[3] The lower limb of an astronomical object is always red.
A green rim is very thin, and is difficult or impossible to see with the naked eye. In usual conditions a green rim of an astronomical object gets fainter, when an astronomical object is very low above the horizon because of atmospheric reddening,[4] but sometimes the conditions are right to see a green rim just above the horizon. The following quote describes probably the longest green rim, which at times could have been a green flash, observation. It was seen on and off for 35 long minutes by members of the Richard Evelyn Byrd party from the Little America exploration base in 1934. Often a green rim changes to a green flash and back again during the same sunset. The image below is an illustration of what members of the Richard Evelyn Byrd party from the Little America exploration base may have seen.[5][6]

Green rim and green flashes of the setting sun

SEEN FOR HALF HOUR
"There was a rush for the surface and as eyes turned southward, they saw a tiny but brilliant green spot where the last ray of the upper limb of the sun hung on the skyline. It lasted an appreciable length of time, several seconds at least, and no sooner disappeared than it flashed forth again. Altogether it remained on the horizon with short interruptions for thirty-five minutes.
When it disappeared momentarily it seemed to have been shut off by a tiny spurt, an inequality in the skyline caused by the barrier surface.
"Even by moving the head up a few inches it would disappear and reappear again and after it had finally disappeared from view it could be recaptured by climbing up the first few steps of the antanea [sic] post."Citation needed for quotation.

To see green rim on and off for 35 minutes there had to be so me mirage present.

There's an interesting situation with green rim observing. Green rim is present at every sunset, but it is too thin to be seen with the naked eye. The best time to observe a green rim is about 10 minutes before sunset.[4] It is too early to use any magnification like binoculars or a telescope to look right at the Sun. (Of course, a magnified image might be projected onto a sheet of paper for safe viewing.) When the sun gets closer to the horizon, the green rim is becoming fainter because of atmospheric reddening.[4] According to the above it is probably correct to conclude that although a green rim is present during every sunset, a green flash is more rare because it requires a mirage to be present.

References

  1. ^ a b c Young, A. (2006). "Green flashes at a glance". http://mintaka.sdsu.edu/GF/papers/Zenit/glance.html. Retrieved 2009-03-05. 
  2. ^ "The Green Flash, BBC Weather online. Retrieved on 2009-05-07.
  3. ^ Dispersive refraction by webexhibits.org.
  4. ^ a b c Green and red rims by Andy Young.
  5. ^ Owen, R (1929). San Francisco Chronicle. p. 5. 
  6. ^ Andrew, Young. Annotated bibliography of mirages, green flashes, atmospheric refraction, etc.. http://mintaka.sdsu.edu/GF/bibliog/bibliog.html. 

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