Mirage of astronomical objects

Last updated
A mock mirage of the setting Sun Mock mirage of the setting sun.jpg
A mock mirage of the setting Sun

A mirage of an astronomical object is a meteorological optical phenomenon, in which light rays are bent to produce distorted or multiple images of an astronomical object. The mirages might be observed for such celestial objects as the Sun, the Moon, the planets, bright stars, and very bright comets. The most commonly observed of these are sunset and sunrise mirages.

Contents

Mirages versus refraction

Mirages are distinguished from other phenomena caused by atmospheric refraction. One of the most prominent features of mirages is that a mirage might only produce images vertically, not sideways, while a simple refraction might distort and bend the images in any way.

The distortion in both images displayed in this section was caused by refraction, but while the image on the left, which is a mirage, demonstrates only vertical distortion, the image on the right demonstrates distortion in all the ways possible. It is easier to see the vertical direction of the mirage not even at the mirage of the Sun itself, but rather at the mirage of a sunspot. As a matter of fact, it is at least a three-image mirage of a sunspot, and all these images show a clear vertical direction.

Superior mirage (3-image mirage) of sunspot #930 Sunspot Mirage.JPG
Superior mirage (3-image mirage) of sunspot #930
An image of the Golden Gate Bridge is refracted and bent by droplets of water. GGB reflection in raindrops.jpg
An image of the Golden Gate Bridge is refracted and bent by droplets of water.

Inferior mirage of astronomical objects

Inferior mirage of comet C/2006 P1 McNaught Inferior mirage of sunset comet.jpg
Inferior mirage of comet C/2006 P1 McNaught
Etruscan vase stage of inferior mirage sunset in Hawaii Sunset inferio mirage.jpg
Etruscan vase stage of inferior mirage sunset in Hawaii
Omega Sun stage of inferior mirage sunset in Hawaii Omega Sun inferior mirage.jpg
Omega Sun stage of inferior mirage sunset in Hawaii

Inferior mirage of astronomical objects is the most common mirage. Inferior mirage occurs when the surface of the Earth or the oceans produces a layer of hot air of lower density, just at the surface. There are two images, the inverted one and the erect one, in inferior mirage. They both are displaced from the geometric direction to the actual object. While the erect image is setting, the inverted image appears to be rising from the surface.

The shapes of inferior mirage sunsets and sunrises stay the same for all inferior mirage sunsets and sunrises. One well-known shape, the Etruscan vase, was named by Jules Verne. [1] As the sunset progresses the shape of Etruscan vase slowly changes; the stem of the vase gets shorter until the real and the miraged Suns create a new shape – Greek letter omega Ω. The inferior mirage got its name because the inverted image appears below the erect one. [2]

Here's how Jules Verne describes an inferior mirage sunset. [1]

All eyes were again turned towards the west. The sun seemed to sink with greater rapidity as it approached the sea ; it threw a long trail of dazzling light over the trembling surface of the water ; its disk soon changed from a shade of old gold, to fiery red, and, through their half-closed eyes, seemed to glitter with all the varying shades of a kaleidoscope. Faint, waving lines streaked the quivering trail of light cast on the surface of the water, like a spangled mass of glittering gems. Not the faintest sign of cloud, haze, or mist was visible along the whole of the horizon, which was as clearly defined as a black line traced on white paper. Motionless, and with intense excitement, they watched the fiery globe as it sank nearer and nearer the horizon, and, for an instant, hung suspended over the abyss. Then, through the refraction of the rays, its disk seemed to change till it looked like an Etruscan vase, with bulging sides, standing on the water.

On very rare occasions the mirages of astronomical objects other than the Sun and the Moon might be observed. An apparent magnitude of an astronomical object should be low enough (that is, bright enough) in order to see it as not only a real object, but also a miraged one.

Mock mirage of astronomical objects

Pancake-like shape of the setting Sun in a mock mirage Sunset mirage 111505.jpg
Pancake-like shape of the setting Sun in a mock mirage

A mock mirage of astronomical objects is much more complex than an inferior mirage. While an inferior mirage of astronomical objects can produce only two images, a mock mirage can produce multiple miraged images. The shapes of the miraged object are changing constantly and unpredictably. In order for a mock mirage to appear, the cooler air needs to be trapped below the inversion. Several inversion layers produce multiple pancake-like shapes. [3]

It is possible that the solar anomaly mentioned in the Book of Joshua may have been an example of a mock mirage. [4] In that tale, Joshua launched a surprise attack on the Amorites following a night march, causing the Amorites to panic and flee as far as Beth-horon, but they did not find a safe haven there. "...they were more who died with the hailstones than they whom the children of Israel slew with the sword." [5] Hailstones are a rare event in deserts and are a good precondition for creating a mock/superior mirage of the setting sun. Inferior mirage is the most common mirage in the deserts. When the Israelites went from a hot desert to a hail-covered desert to fight the Amorites, the inversion layers could have created a mock mirage of the setting sun. To the Israelites, the sun would then have appeared to stand still. [4] A poem is quoted from the Book of Jasher, which states that the Sun stood still at Gibeon, and the Moon in the valley of Ajalon, in order that Joshua could complete the battle. [6]

Joshua commands the Sun to stand still in the sky Dore joshua sun.jpg
Joshua commands the Sun to stand still in the sky

10.12 Then spoke Joshua to the LORD in the day when the LORD delivered up the Amorites before the children of Israel; and he said in the sight of Israel: 'Sun, stand thou still upon Gibeon; and thou, Moon, in the valley of Aijalon.
10.13 And the sun stood still, and the moon stayed, until the nation had avenged themselves of their enemies. Is not this written in the book of Jashar? And the sun stayed in the midst of heaven, and hasted not to go down about a whole day. [6]

Mock mirage of the setting Moon Mock mirage of the setting Moon.jpg
Mock mirage of the setting Moon

Novaya Zemlya effect

Due to a normal atmospheric refraction, sunrise occurs shortly before the Sun crosses above the horizon. Light from the Sun is bent, or refracted, as it enters Earth's atmosphere. This effect causes the apparent sunrise to be earlier than the actual sunrise. Similarly, apparent sunset occurs slightly later than actual sunset.

In ordinary atmospheric conditions, the setting or rising Sun appears to be about half a degree above its geometric position. But sometimes, very unusual atmospheric circumstances can make it to be visible when it is really between two and five degrees below the horizon. This is called the Novaya Zemlya effect, because it was first observed in Novaya Zemlya, where the Sun was seen when, according to astronomical calculations, it should have been two degrees below the horizon.

However, due to changes in air pressure, relative humidity, and other quantities, the exact effects of atmospheric refraction on sunrise and sunset time cannot be predicted. Also note that this possible error increases with higher (closer to the poles) latitudes. [7]

This mock mirage sunset was photographed in San Francisco four minutes later than apparent sunset time. It cannot be considered the Novaya Zemlya effect, yet it gives a good visual representation of what Fridtjof Nansen may have seen when he was observing the phenomenon. Complex mock mirage sunset.jpg
This mock mirage sunset was photographed in San Francisco four minutes later than apparent sunset time. It cannot be considered the Novaya Zemlya effect, yet it gives a good visual representation of what Fridtjof Nansen may have seen when he was observing the phenomenon.

Novaya Zemlya is a polar region in Russia. The Novaya Zemlya effect is a mirage caused by high refraction of sunlight between atmospheric thermoclines. The Novaya Zemlya effect will give the impression that the sun is rising earlier than it actually should or the sun is setting later than it actually should.

Fridtjof Nansen wrote [8] [9]

The mirage was at first like a flattened-out glowing red streak of fire on the horizon; later there were two streaks, one above the other, with a dark space between; and from the main-top I could see four, or even five, such horizontal lines directly over one another, and all of equal length; as if one could only imagine a square dull-red sun with horizontal dark streaks across it. An astronomical observation we took in the afternoon showed that the sun must in reality have been 2° 22' below the horizon at noon; we cannot expect to see its disk above the ice before Tuesday at the earliest; it depends on the refraction, which is very strong in this cold air.

It is possible to observe the Novaya Zemlya effect in any place, where the temperature variations are great enough to produce a high refraction.

Green flash

Green flash is a rare optical phenomenon that occurs during or shortly after set and during or before rise of a bright astronomical object, when a green spot is visible for a short period of time above a mirage of an astronomical object or its set/rise point. Green flashes are enhanced by atmospheric inversions which increase the density gradient in the atmosphere, and therefore increase refraction. In other words, to see a green flash a mirage should be present. [10]

Jules Verne described a green flash. [1] [11]

...it will be ' green,' but a most wonderful green, a green which no artist could ever obtain on his palette, a green which neither the varied tints of vegetation nor the shades of the most limpid sea could ever produce the like ! If there be green in Paradise, it cannot but be of this shade, which most surely is the true green of Hope !

the incomparable tint of liquid jade

Many tend to believe that seeing a green flash brings good luck. [12]

Green flash Green flash in san francisco.jpg
Green flash

Stories are told,
By Sailors of old,
Who sought more than distant shore.
When looking asea
Alert ye be,
And by chance ye might see more.

At setting sun
When day is done,
While lanyards ye do lash.
Where sea meets sky
Keep watchful eye
For the Mystical Green Flash.

If luck be there
And it catch your stare,
Your fortune turns my mate.
Night sky is red
Smooth sail ahead,
A charmed life is your fate.

Sure as Neptune guides
The ocean tides,
Where his dolphins leap and splash.
Favorable days
Await those who gaze
'Pon the Mystical Green Flash.

Sunset sequence with two green flashes in the second and fourth frames Sunset sequence07-23-06.jpg
Sunset sequence with two green flashes in the second and fourth frames

Green flashes might be observed from any place with a low horizon. Deserts, oceans and ice shelves are probably the best places to observe mirages and therefore green flashes. It is easier not to miss a green flash during sunset than during sunrise. It is especially true regarding an inferior mirage green flash, when the timing should be just right to capture it at sunrise. [13]

I could see the sun glowing below the distant horizon. Then, for what seemed like at least a second, the green flash flooded the desert like an alien heliograph. A moment later, the skyline erupted with the instant magnificence of the sun, its sudden warmth.

From the above observation it is clear that the author observed an inferior mirage green flash, when the much warmer surface of the desert with the help of the rising Sun was fighting the cool morning air, producing in the process a green flash – one of nature's great spectacles.

A green flash might be also seen with a rising or setting Moon.

In the right conditions it is common to observe multiple green flashes during one mock mirage sunset.
Some claim they saw a green flash from Venus. This may be true, but it might be that a color of the setting or the rising planet is mistaken for a real green flash that is a by-product of a mirage. [14]

Green rim

The upper rim of the Sun is green while the lower rim is red in this image taken as the Sun sets behind the Golden Gate Bridge. Green rim of the setting sun.jpg
The upper rim of the Sun is green while the lower rim is red in this image taken as the Sun sets 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. [15] The lower limb of an astronomical object is always red.

The 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, [16] but sometimes the conditions are right to see a green rim just above the horizon.

The following quote describes probably the longest observation of a green rim, which sometimes could have been a green flash. Members of Richard E. Byrd's party from the Little America exploration base saw the phenomenon on and off for 35 minutes (source for 30 versus 35 minutes?).

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.

Green rim and green flashes of the setting Sun Green rim and green flashes in SF.jpg
Green rim and green flashes of the setting Sun

Often the green rim of the setting Sun will change to a green flash and then back again to a green rim during the same sunset. The image to the right might accurately illustrate what members of Byrd's party from the Little America base might have seen. [9] [17]

However, to see a green rim and green flash on and off for 35 minutes, there must have been some degree of mirage present.

A green rim is present in every sunset, but it is too thin to be seen with a naked eye. The best time to observe the green rim is about 10 minutes before sunset time. [16] However, the solar disc is too bright at that time to use magnification, such as binoculars or telescopes, to look directly at the Sun. Of course, a telescope or binoculars image can be projected on a sheet of paper for viewing. When the Sun gets closer to the horizon, the green rim gets fainter because of atmospheric reddening. [16] Although a green rim is present in every sunset, and a green flash is rare because it requires a mirage to be present, it is actually more common for people to have seen a green flash rather than a green rim.

Not a mirage

Different shapes of the setting Sun Shapes of the sun due to clouds and vog.jpg
Different shapes of the setting Sun
The second Sun at the image is the inter-reflection of the Sun from camera lens, and not a mirage Digital camera artifact.jpg
The second Sun at the image is the inter-reflection of the Sun from camera lens, and not a mirage

The composite image on the left is made out of five frames of different sunsets. None of the images is a mirage. Frames # 1 and # 2 could fool even a very experienced observer. They do look like a mock mirage of the setting Sun, but they are not. Frames #3 and # 4 are clearly not a mirage. Frame # 5 is not a mirage and not even a sunspot, it is a spider with the Sun as a background. The strange shapes of the Sun in this composite is due to vog and clouds.[ citation needed ]

Numerous atmospheric effects, such as vog, clouds, smoke, smog and others could generate a mirage like appearance of an astronomical object.[ citation needed ] Lens flares and ghost images also might be responsible for a false mirage or a false green flash.[ citation needed ]

See also

Related Research Articles

A solar equinox is a moment in time when the Sun crosses the Earth's equator, which is to say, appears directly above the equator, rather than north or south of the equator. On the day of the equinox, the Sun appears to rise "due east" and set "due west". This occurs twice each year, around 20 March and 23 September.

<span class="mw-page-title-main">Atmospheric duct</span> Horizontal layer that propagates electromagnetic radiation

In telecommunications, an atmospheric duct is a horizontal layer in the lower atmosphere in which the vertical refractive index gradients are such that radio signals are guided or ducted, tend to follow the curvature of the Earth, and experience less attenuation in the ducts than they would if the ducts were not present. The duct acts as an atmospheric dielectric waveguide and limits the spread of the wavefront to only the horizontal dimension.

<span class="mw-page-title-main">Green flash</span> Meteorological optical phenomenon

The green flash and green ray are meteorological optical phenomena that sometimes occur transiently around the moment of sunset or sunrise. When the conditions are right, a distinct green spot is briefly visible above the Sun's upper limb; the green appearance usually lasts for no more than two seconds. Rarely, the green flash can resemble a green ray shooting up from the sunset or sunrise point.

<span class="mw-page-title-main">Horizontal coordinate system</span> Type of celestial coordinate system

The horizontal coordinate system is a celestial coordinate system that uses the observer's local horizon as the fundamental plane to define two angles: altitude and azimuth. Therefore, the horizontal coordinate system is sometimes called the az/el system, the alt/az system, or the alt-azimuth system, among others. In an altazimuth mount of a telescope, the instrument's two axes follow altitude and azimuth.

<span class="mw-page-title-main">Inversion (meteorology)</span> Deviation from the normal change of an atmospheric property with altitude

In meteorology, an inversion is a deviation from the normal change of an atmospheric property with altitude. It almost always refers to an inversion of the air temperature lapse rate, in which case it is called a temperature inversion. Normally, air temperature decreases with an increase in altitude, but during an inversion warmer air is held above cooler air.

<span class="mw-page-title-main">Mirage</span> Naturally occurring optical phenomenon

A mirage is a naturally-occurring optical phenomenon in which light rays bend via refraction to produce a displaced image of distant objects or the sky. The word comes to English via the French (se) mirer, from the Latin mirari, meaning "to look at, to wonder at".

<span class="mw-page-title-main">Sunrise</span> Time of day when the sun appears above the horizon

Sunrise is the moment when the upper rim of the Sun appears on the horizon in the morning. The term can also refer to the entire process of the solar disk crossing the horizon.

<span class="mw-page-title-main">Sunset</span> Daily falling of the Sun below the horizon

Sunset is the disappearance of the Sun below the horizon of the Earth due to its rotation. As viewed from everywhere on Earth, it is a phenomenon that happens approximately once every 24 hours except in areas close to the poles. The equinox Sun sets due west at the moment of both the spring and autumn equinoxes. As viewed from the Northern Hemisphere, the Sun sets to the northwest in the spring and summer, and to the southwest in the autumn and winter; these seasons are reversed for the Southern Hemisphere.

<span class="mw-page-title-main">Sky</span> View upward from the surface of the Earth

The sky is an unobstructed view upward from the surface of the Earth. It includes the atmosphere and outer space. It may also be considered a place between the ground and outer space, thus distinct from outer space.

<span class="mw-page-title-main">Twilight</span> Atmospheric illumination by the Sun below the horizon

Twilight is light produced by sunlight scattering in the upper atmosphere, when the Sun is below the horizon, which illuminates the lower atmosphere and the Earth's surface. The word twilight can also refer to the periods of time when this illumination occurs.

<span class="mw-page-title-main">Atmospheric refraction</span> Deviation of light as it moves through the atmosphere

Atmospheric refraction is the deviation of light or other electromagnetic wave from a straight line as it passes through the atmosphere due to the variation in air density as a function of height. This refraction is due to the velocity of light through air decreasing with increased density. Atmospheric refraction near the ground produces mirages. Such refraction can also raise or lower, or stretch or shorten, the images of distant objects without involving mirages. Turbulent air can make distant objects appear to twinkle or shimmer. The term also applies to the refraction of sound. Atmospheric refraction is considered in measuring the position of both celestial and terrestrial objects.

<span class="mw-page-title-main">Novaya Zemlya effect</span> Atmospheric optical phenomenon

The Novaya Zemlya effect is a polar mirage caused by high refraction of sunlight between atmospheric thermal layers. The effect gives the impression that the sun is rising earlier than it actually should, and depending on the meteorological situation, the effect will present the Sun as a line or a square — sometimes referred to as the rectangular sun — made up of flattened hourglass shapes.

<span class="mw-page-title-main">Fata Morgana (mirage)</span> Optical phenomenon

A Fata Morgana is a complex form of superior mirage visible in a narrow band right above the horizon. The term Fata Morgana is the Italian translation of "Morgan the Fairy". These mirages are often seen in the Italian Strait of Messina, and were described as fairy castles in the air or false land conjured by her magic.

<span class="mw-page-title-main">Belt of Venus</span> Atmospheric phenomenon

The Belt of Venus is an atmospheric phenomenon visible shortly before sunrise or after sunset, during civil twilight. It is a pinkish glow that surrounds the observer, extending roughly 10–20° above the horizon. It appears opposite to the afterglow, which it also reflects.

<span class="mw-page-title-main">False sunrise</span> Atmospheric optical phenomena in which the Sun appears to have risen

A false sunrise is any of several atmospheric optical phenomena in which the Sun appears to have risen, but is actually still some distance below the horizon. A number of different atmospheric conditions can be responsible for this effect, all of which divert the sunlight in such a way as to allow it to reach the observer's eye, thereby giving the impression that the light comes directly from the Sun itself. The spread of light can sometimes be deceivingly similar to a true sun.

<span class="mw-page-title-main">Looming and similar refraction phenomena</span>

While mirages are the best known atmospheric refraction phenomena, looming and similar refraction phenomena do not produce mirages. Mirages show an extra image or images of the miraged object, while looming, towering, stooping, and sinking do not. No inverted image is present in those phenomena either. Depending on atmospheric conditions, the objects can appear to be elevated or lowered, stretched or stooped. These phenomena can occur together, changing the appearance of different parts of the objects in different ways. Sometimes these phenomena can occur together with a true mirage.

<span class="mw-page-title-main">Atmospheric optics</span> Study of the optical characteristics of the atmosphere or products of atmospheric processes

Atmospheric optics is "the study of the optical characteristics of the atmosphere or products of atmospheric processes .... [including] temporal and spatial resolutions beyond those discernible with the naked eye". Meteorological optics is "that part of atmospheric optics concerned with the study of patterns observable with the naked eye". Nevertheless, the two terms are sometimes used interchangeably.

A false sunset can refer to one of two related atmospheric optical phenomena, in which either (1) the Sun appears to be setting into or to have set below the horizon while it is actually still some height above the horizon, or (2) the Sun has already set below the horizon, but still appears to be on or above the horizon. Depending on circumstances, these phenomena can give the impression of an actual sunset.

<span class="mw-page-title-main">Antarctic Circle</span> Boundary of the Antarctic

The Antarctic Circle is the most southerly of the five major circles of latitude that mark maps of Earth. The region south of this circle is known as the Antarctic, and the zone immediately to the north is called the Southern Temperate Zone. South of the Antarctic Circle, the Sun is above the horizon for 24 continuous hours at least once per year and the centre of the Sun is below the horizon for 24 continuous hours at least once per year ; this is also true within the equivalent polar circle in the Northern Hemisphere, the Arctic Circle.

<span class="mw-page-title-main">Long distance observations</span> Observation of distant objects on Earths surface or terrestrial features

Long-distance observation is any visual observation, for sightseeing or photography, that targets all the objects, visible from the extremal distance with the possibility to see them closely. The long-distance observations can't cover:

References

  1. 1 2 3 Jules Verne (1883). The Green Ray. Translated by M. de Hauteville. S. Low, Marston, Searle, and Rivington. p.  305. sun.
  2. An Introduction to Mirages by Andy Young
  3. Sunset Mirages Les Cowley
  4. 1 2 Camuffo, D (March 1990). "A meteorological anomaly in Palestine 33 centuries ago: How did the sun stop". Theoretical and Applied Climatology. Springer Wien. 41 (1): 81–85. Bibcode:1990ThApC..41...81C. doi:10.1007/BF00866205. S2CID   118192305.
  5. The Book of Joshua 10.11 Joshua
  6. 1 2 The Book of Joshua 10.13 Joshua
  7. "Solar Calculator Glossary". NOAA.gov.
  8. Nansen, Fridtjof (1897). Farthest North. New York: Harper & Brothers. pp. 394–395.
  9. 1 2 Andrew, Young. Annotated bibliography of mirages, green flashes, atmospheric refraction, etc.
  10. Explaining Green Flashes by Andy Young
  11. Jules Verne (1883). The Green Ray. Translated by M. de Hauteville. S. Low, Marston, Searle, and Rivington. p.  32. green ray.
  12. K. Solarino : The Green Flash Collection
  13. Twigger, Robert. "Egyptology News". egyptology.blogspot.com.
  14. "Green Flash from Venus" (PDF). NOAA.gov.
  15. "Dispersive refraction". WebExhibits.
  16. 1 2 3 Young, Andy. "Green and red rims".
  17. Owen, R. (1929). "San Francisco Chronicle". p. 5.