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Astronomy, Optics, Panoramas

Several important reasons why you should see the 2026 solar eclipse

Aurora and total solar eclipse

Pic. 8 The photomontage depicting the aurora occurrence at the same time when totality occurs. This is an assumed view from eastern part of Taymyr penninsula, where totality falls at midnight sun on August 12/13 2026. We are considering the auroral structures at the same section of sky where eclipse occurs.

It’s still quite a lot of time to the 2026 total solar eclipse event, which has been already considered by myself in terms of the possibility of seeing its impact in the atmosphere when the phenomenon happens below the horizon.  However, the character of this path of totality requires attention far earlier than normal, as this type of situation doesn’t happen often.
The 2026 total solar eclipse is going to be specific due to several reasons, which I am going to explain in this article. All these reasons have their scientific background. Some of them could be also pioneers, observed presumably the first time in history, taking into account the utter lack of any reports and nowadays also images. The essence of all these sides phenomena going along with the totality event seems to be not only the proper attention but also involvement of a dozen or so observers, able to manage with this certain moment from different locations. I hope, that after reading this full article you will understand better my scientific intentions regarding the forthcoming unique total solar eclipse on August 12, 2026.
Before I start describing all these eclipse-related circumstances, we all should know how the 2026 total solar eclipse will look like in the geometrical sense.


The primary factor, which decides about the nature of the totality path observed (or not) from the Earth’s surface is Gamma. The Gamma factor describes how the lunar (or Earth’s) shadow falls at the other body against its central alignment. Otherworldly the Gamma factor describes any “distance” of the shadow cone axis from the center of the celestial body (Earth in our case). This distance is measured as a fraction of the equatorial radius of the given celestial body. If the Earth radius counts roughly 6378km ( at the equator, although for sake of simplification we can consider Earth as the perfect sphere), it will mean, that for Gamma value 0,01 the shadow hits Earth around 64km north from the center of the planet. The center of the planet is the point, where the Sun is observed roughly overhead. It’s also important to know, that positive Gamma values mean north direction and negative south.
In order to understand the Gamma factor better, we should discuss where does it come from. For sake of simplification, we can assume, that for our current case the Gamma value is exactly 0, where the Earth’s center passes exactly through the axis of the lunar umbra. Now we could be curious how the situation will look exactly a saros later.  The saros is the period between two successive very similar eclipses or the period when the Sun, Earth, and Moon return to the same relative geometry. The length of the saros is 6585.3 days (18 years 11 days and 8 hours). After this period roughly, we can observe the Sun, Earth, and Moon at pretty much the same configuration. However, the saros period should be considered not only as the 223 synodic months period but also as the 242 nodal months (draconic months). The draconic months is the average period between two consecutive transits of the Moon through the same node. Because the lunar orbit is tilted about 5.14° against the ecliptic plane, it crosses this plane twice a month – during the ascending and descending nodes. The last lunar month which comprises the changing Gamma value is the anomalistic month, which corresponds to the perigee to perigee period. The position of the line of lunar apsides spins around its axis in about 3233 days (8.85 years), which means that the Moon will take a longer journey between one perigee and another, which is called the anomalistic month. Concluding, these three types of lunar months are not perfectly commensurate with one another. It turns the particular moment in the given saros slightly different than a saros earlier or later. In practice, the Moon’s node shifts about 0.48º eastwards with each saros cycle. In terms of the eclipses, we consider the saros cycle, which includes all the lunar saros resulting in any eclipse occurrence both lunar or solar. Usually, the saros series begins when the New Moon occurs about 17-18º east of the node. Then the average absolute gamma value is +1.55. Being granular, it varies between 1.53 (for total solar eclipses) and 1.57 (for annular solar eclipses). The lunar shadow misses Earth at about 3500km distance. If the absolute value of the Gamma is equal to or lower than mentioned earlier, the eclipse is visible from the Earth’s surface, usually somewhere nearby polar regions. For a lunar eclipse, if the absolute Gamma value is higher than 1.55, the penumbra misses the lunar surface completely.  At the second saros, the lunar shadow falls about 250-300km closer to Earth, which will result in a slightly larger eclipse magnitude observed. Next, after about 10 saros cycles (over 180 years) the shadow or antumbra will occur near the pole. After another about 700-1000 years, the central solar eclipse will be observed, however, every single saros will make them displaced with respect to the Earth’s center by about 250-300km. After other several ages, the shadow occurs at the opposite polar region and leaves the Earth’s surface in the successive saros. The last 10 saros periods round off the saros cycle effectively, as the penumbra goes gradually away from our planet. Another Gamma value variation is related to Earth’s position against the Sun. It was found, that the Gamma value changes tend to be larger when Earth passes its aphelion. In the opposite configuration – the perihelion, the Sun’s apparent motion is higher and may reduce the eastward shift of the node. This situation is driven by the eccentricity of Eart’s orbit. Formerly it causes even reversing the direction of the Gamma value for nodes falling around the moment of perihelion.
Regarding the saros 126, which part is the 2026 total solar eclipse (occurring at descending node), we should consider also another feature, typical for high absolute gamma values. Looking at the pattern below, as well as here we can see the gamma value relation with the solar azimuth, at which the greatest eclipse takes place.

Saros 126 solar eclipse Espenak Meeus

Pic. 1 The Saros 126 including 2026 total solar eclipse (

For eclipses with gamma absolute value about 0.9 and higher, we can see the umbral path movement just at one part of the day (morning or afternoon) instead of throughout a whole day (from sunrise to sunset).  In order to grasp it better, I presented the examples below, which include 3 eclipses  (Pic. 2).

Relation the path of totality with the Gamma value

Pic. 2 The relation of the Path of totality with the Gamma value. For absolute Gamma values (optionally) higher than 0.9 the eclipse event is confined to one part of the day only. In practice, it may start in the morning and finish yet in the morning or at most in the middle of the day unlike the eclipses located closer to the Earth center, which paths proceed from the morning (sunrise) to the evening (sunset). For the 2026 total solar eclipse, where the Gamma value is just a tad lower than 0.9, the solar azimuth at the greatest eclipse barely exceeds the cardinal north direction. In turn, the whole event falls in the afternoon time ( Click to enlarge.

Obviously, the Gamma value is not only one factor here, and all the geometry aspects related to this situation as well as the general shape of the umbral (or antumbral) path across the Earth’s surface will be definitely explained in the future. This thread is much longer and requires a separate paper to a detailed explanation of all these components. For the 2026 total solar eclipse, it’s enough to know how the high gamma value shapes the Moon’s shadow way in the considered part of the Globe.
The 2026 total solar eclipse will occur in the northern hemisphere and almost a whole event will take place during the afternoon hours. This is the specificity of this eclipse as shown in the pattern above (Pic. 2) and below (Pic. 3).

2026 Total Solar eclipse graphic path

Pic. 3 The graphic pattern of the 2026 total solar eclipse (

The eclipse begins briefly after midnight local time and shifts shortly towards the western sky sphere where participates as the afternoon event upon its disappearance at sunset east of Balearic Islands. The High absolute Gamma value means also the deep partial eclipse in the areas beyond the eclipse path. Due to Earth’s curvature, the distance between the areas with a certain eclipse magnitude is longer between the umbral path and terminator line than outside of the umbral path. Considering the 2026 total solar eclipse, all the areas located beyond the path of the shadow will experience the deep partial eclipse with a magnitude of at least 0.83. Umbra will move close to the northern limit of Earth’s disk, although due to descending node combined with summertime in the northern hemisphere, the central duration will fall a bit south, as you can see in the attached video below. The video clearly depicts the umbral movement at the descending node, which could be seen by an observer standing on the Moon.

The simulation of 2026 total solar eclipse for an assumed observer standing on the Moon (credits: Domick Ford/

Watching the simulation above, you can better understand what I meant by writing “beyond the umbral path”. It’s the area between the path of totality and Earth’s terminator defined here by its limb.  This part of the planet will be shaded by a deep penumbra, which will make it relatively darker than the area located outside of the eclipse path, towards the geometric center. The smaller amount of light in that areas will be caused not only by the eclipse magnitude but also by the low altitude of the Sun. In turn, will be the difference between the area falling within i.e. 0.9 eclipse magnitude and the same area on the other side of the umbral path. It may be noticeable in sky surface brightness measurements.
Another thing is the quite significantly curved path of totality, which is predominantly driven by Earth rotation. It’s also the subject of detailed explanation in the future.
After this sample of geometry, the essence of the 2026 total solar eclipse should be more clarified for you.


In terms of the rareness of the 2026 total solar eclipse, which arose out of its geometry discussed earlier, there are several valuable optical responses possible to watch both within the path of totality as well as within the illuminated atmosphere of our planet. They were listed and described below in detail.

I. TOTAL SOLAR ECLIPSE AND AURORA BOREALIS (NORTHERN RUSSIA) – In the theoretical sense it could be the best occasion to see these two spectacular phenomena at once. I don’t want to conjure you, that it’s fairly possible, especially without any reasonable explanation of the aurora occurrence.
If we want to consider the visibility of the total solar eclipse and aurora borealis at once, we should have some knowledge about the brightness relation between the sky during the total solar eclipse and the maximum possible brightness of the aurora. The aurora is caused by the interaction of the atmospheric gases with the solar wind particles. Otherworldly it’s a collision between energetic electrons and molecules in the Earth’s ionosphere. As a result, we can see a beautiful display of the lights in the sky, where oxygen gives the green and red light and nitrogen a blue and purple light accordingly.

Aurora oval and Earths magnetosphere

Pic. 4 Auroral oval and Earth’s magnetosphere. A brief explanation of how the aurora is produced (

The brightness of the Aurora, same as the airflow is defined by the International Brightness Coefficient (IBC) – the convenient logarithmic classification system, which includes effectively 5 levels of light radiance expressed in the Rayleigh (precisely – the kiloRayleigh – kR) units. The Rayleigh is a radiometric unit, which defines the photon flux and measures a faint light emitted in the sky. In order to better understanding the Rayleigh radiometric measurements, it’s vital to convert them to some photometric units, as discussed in this article.  Conversion between radiometric and photometric units is not straightforward due to the spatial distribution of light, which plays a pivot role here. The biggest correspondence of the Rayleigh unit can be with the S10vis unit, which measures the intensity (surface brightness) corresponding to one star of 10th (visual) magnitude per square degree of the sky (Kraus, Mc-Graw Hill, 1966).  Turning the S10vis unit, we should receive 6.9 * 10-7 Nits – 0,00000069 Nits. The Nit replaces the basic SI unit for luminance, which is candela per square meter (cd/m2), and defines how much light an object emits. The Lux unit measures how much light is received from an object (Pic. 5).

Nit vs Lux

Pic. 5 Relation between Nit and Lux units. Lux defines the illumination of the light source, whereas Nit says about the illumination of the surface reflecting this light. These values can be used interchangeably in some situations when the light is reflected more than once.

If we want to receive the number of Lux from Nits, we should multiply the Nits by the Pi value. If in our case the S10vis unit counts 0.00000069 nits then 0.00000069*3.3.14159 = 0.0000021676971 Lux.
1 Rayleigh unit should correspond to 0.07 S10vis units. In this case, the 1 Rayleigh will be equal to 0.000000151738797 Lux.  In this transformation, we also should remember about the Angstrom – a metric unit of length, which is also used for measuring the visible light wavelength (between 4000 and 7000A). The aforementioned conversion applies to monochromic radiation at 5577A, which as a standard reference corresponds to a strong green oxygen line (Omholt, 1971). We obviously have some exceptions, where aurora might have the red border or shine in red, although for our concerns, we can take the green oxygen as the primary color of this phenomenon.
Another, the closer approach can be played between the S10vis and mag/arcsec2 unit, as both of them measure the surface brightness.  In extreme cases (estimation for diffused galactic light), the surface brightness might be as low as 9 S10vis unit, being equal to +25mag/arcsec2.

Having this basic knowledge about the transformation between the radiometric and photometric units, we can finally describe the classification of aurora brightness.
The first level (IBC0) applies basically the situation when the human eye is unable to see the shining object (or area) properly, being defined as the “subvisual”. It’s related predominantly to the night sky (except for stars and other celestial bodies), which intensity reaches about 250R along with the corresponding radiance at 557.7mm (Shaw et al., 2009) or alternatively. The aurora brightness is classified between 4 remaining IBC levels, where:
IBC1 – corresponds to the faintest and usually, patchy aurora, which is about 3-4 times brighter than the normal airglow (Mieghem, 1961). It describes the aurora activity up to 2 Kp-index. This scale is equal to the object or area of the sky, which has a white appearance.  A good example here can be the Milky Way, in which predominant light radiance is equal to 1kR (upwards to a few kR) or 70 S10vis unless we considering the galactic equator, which lifts up these values to the range between 160 and 640 S10vis. This level remains mostly beyond the ability of human vision when an observer is located in the light-polluted area. The surface brightness varies here between +23,5 and +21,5 mag/arcsec2.
IBC2 – this level features the commencement of color vision, obviously under the sky free of light pollution. Here the observed aurora looks like a homogeneous arc. This level corresponds to about 10kR or 700 S10vis  brightness indicating i.e. thin moonlit cirrus clouds. The surface brightness, in this case, hovers around +21mag/arcsec2. The aurora activity corresponds here to the 3 Kp-index with pale green coloration visible.
IBC3 – this level corresponds usually to a bright display i.e. moonlit cumulus cloud. The brightness here reaches 100kR or 7000 S10vis or the range between +19 and +18 mag/arcsec2. In the case of the aurora, we can see a bright and colorful aurora display, which bright stars don’t shine through, as it reaches and 0.0151738797 Lux brightness, like twilight glow when Sun is about 11 degrees below the horizon. It can be the 5-7 Kp-index with constant display and obvious coloration. It does happen quite often in polar regions.
IBC4 – The brightest level, where at the extreme cases the light intensity might be equal to full moonlight, reaching about 1000kR or 70000 S10vis with surface brightness reaching about +16mag/arcsec2. In turn, the objects are bright enough to cast the shadow, which means total illumination of the scene. The occurrence of such bright aurora is rare, unfortunately. If occurs for 8-9 Kp-index. The brightest auroras can reach 0.151738797 Lux, whereas the overhead full Moon illuminance is 0.267 Lux. In practice, this value will be equal to the twilight glow when Sun is around 8,5 degrees below the horizon.  In extremely rare cases an observer can read the newspaper, as happens in 1859 where some people were even awoken by auroral light (Green et al., 2006) or in East Asia in 1770 being “As bright as a night with a full moon” (Ebihara et al., 2017). Everything is possible when we have no light pollution or moonlight. Aurora can shine through thin clouds too. The extremely bright auroras happen when we experience the discrete auroras.  They usually form as discrete auroral arcs and can be found deep inside the aurora oval or at the poleward border of the wide (so-called double) auroral oval (Yahnin et al., 1997). The auroral oval is a narrow horizontal band of light up to hundreds of kilometers long, usually oriented from geomagnetic east to west (Considine, 2005).
The aurora represents some specific forms, featuring their own particular emission lines and bands, therefore it’s hard to translate the intensity of aurora to total emission, thereby hard to measure the brightness. On the other hand intensity of a particular auroral form depend on the direction, from which it is observed (Omholt, 1971).

Next to the brightness, important is also the duration of the aurora. Short-lived aurorae (up to one hour) seem to be much more frequent than long displays (Chamberlain, 1961). This is important from the eclipse point of view because we won’t know until the last time about the aurora’s appearance within the eclipsed section of the sky. On the other hand, short-lived auroras often have big intensity. The greatest concentration of aurora occurs during some brief outbursts with vivid motions of rayed bands. We should also remember the location against the magnetic field lines. Usually, when watching aurora further from the zenith, it can look fairly faint unlike observed directly along the magnetic field lines (Romick, Belon, 1967). The auroral zones encircle the geomagnetic poles at roughly 23 degrees (Omholt, 1971). They appear also within these zones, but with less frequency and intensity. Moving equatorward from the auroral zones, their intensity and frequency fall abruptly. From the big distance, aurora can be perceived as some luminous cloud with certain surface brightness.
The typical development of the aurora along the magnetic fields starts from emerging the homogeneous arc, classified as the IBC2 level and elongated approximately along the E-W direction, which next after at most several hours can turn into an intensive form of bands moving rapidly across the sky. The aurora can shift throughout the entire sky even within minutes. Finally becomes fainter and irregular (Pic. 6).

Auroral break-up Omholt, 1971

Pic. 6 The sequence of auroral development from its beginning to the end (break-up) recorded by all-sky cameras (Omholt, 1971).

The intensity of aurora is primarily caused by sunspots, especially large sunspot groups passing across the solar central meridian as seen from Earth (Craig, 1965). Furthermore, the aurora display tends to recur after about 27 days, which corresponds to the synodic rotation period of the Sun in its low latitudes (Dixon, 1939). Some correlations might be also with the 29.5 days lunar period, however, it’s only explained by much better conditions for aurora observations during the moonless night. The solar sunspots are marked by intensive magnetic activity which is released to the gassy ejection and solar wind. Next, the solar wind shapes the conditions in the magnetosphere. The solar wind varies in intensity and depends on solar activity, which changes in its cycles. Nowadays the Sun entered its 25th solar cycle. Every solar cycle lasts around 11 years and includes solar maximum as the period of greatest activity and solar minimum as the moment of least solar activity in the given period. The solar maximum for the 25th cycle is going to fall around 2025 year (Pic. 7), which is perfect in terms of considering the 2026 totality.

Progression of the sunspots amount throughout the 25th solar cycle (

Pic. 7 The number of sunspots progression throughout the 25th solar cycle (Space Weather Prediction Center/

The prospect of the total amount of sunspots in 2026 is really promising, as we shall expect more than 100 in the 2nd part of the year. It makes a big likelihood for the brightest auroras possible to happen, driven by great magnetic storms. At the time of high activity, the aurora might cover a whole sky poleward or even stretch to the zenith, which would be really beneficial in terms of the eclipse.  We are definitely talking about the Kp-index 8 and 9 auroras, where the Kp-index is the semi-logarithmic scale based on the average variation of the magnetic field (Bone, 2007).
The aurora brightness comparisons made above with its strong correspondence to the brightness of the twilight glow, refer mostly to the sky at the solar direction. The sky located at the zenith is significantly darker, therefore the aurora shouldn’t be washed out at the same moment, as concerned above. For the observer, it should appear earlier after sunset and be visible a bit longer at dawn.
Taking into account the eclipse path location, especially its commencement in northern Russia, the important factor is definitely the magnetic pole location, which travels across the Arctic Ocean (Pic. 8). In 2026 the pole will be located closer to the Severnaja Zemya and Taymyr Penninsula, which is to experience the eclipse as a first near the midnight sun moment.

North magnetic pole prediction upon 2025

Pic. 8 The north magnetic pole prediction upon 2025 (

Therefore, the aurora oval should be pushed southwards. For an observer watching the totality at midnight from the Taymyr Penninsula, aurora presumably could appear at the southern part of the sky, high above the horizon, where the sky is the darkest. Having the fish-eye or wide-angle lens, the observer could be capable to catch the totality and aurora in the same frame (Pic. 9).

Aurora and total solar eclipse

Pic. 9 The photomontage depicting the aurora occurrence at the same time when totality occurs. This is an assumed view from the eastern part of the Taymyr peninsula, where the totality falls at midnight sun on August 12/13 2026. We are considering the auroral structures at the same section of the sky where the eclipse occurs (image based on the totality observed on July 10, 2010, near Coyhaique in Chile, credits: (aurora) and Daniel Fisher/

The totality at Taymyer Penninsula will have very similar geometry to the one observed near Coyhaique in Chile in 2010 (Pic. 9). The most spectacular would be aurora happening just next to the eclipsed Sun as shown above (Pic. 9), however, the sky surface brightness at that direction as well as the aurora oval position should be concerned here.
At this stage is very important to consider the moment of the first (or last) aurora appearance against the twilight. It’s widely assumed, that aurora starts to be clearly visible or possible to detect towards the end of the nautical twilight when the Sun is 12 degrees below the horizon. Obviously, we know, that the end of the nautical twilight is a significant mark for the brightness of the sky, as an observer can see the directly illuminated ozonosphere in the geometrical sense. Regardless of this factor, the nautical twilight is not a decisive moment for the detection of the aurora same as its visual performance. Because the nautical twilight glow reaches at most 0.00806 Lux at its end is not able to draw out the aurora details, unless it appears closer to the solar azimuth and low above the horizon.

The arc of aurora near the end of nautical twilight

Pic. 10 The brilliant arc of aurora at the end of nautical twilight as seen from Greenland (

Aurora nautical twilight

Pic. 11 The string aurora starts to faint when Sun is about 11 degrees below the horizon, what corresponds to near full-moon conditions. It happens especially towards solar azimuth, where sky brightness is very similar to full moon conditions (

The situation starts to change, as the brightness of the nautical twilight glow hovers the full Moon’s brightness. Because the strongest aurora reaches illumination like full Moon, this time is somewhat the barrier marking the moment, when even the strongest aurora becomes visually fainter. In a practical sense, the full Moon doesn’t ruin your chances to see still quite a good aurora event (Pic. 12).

Aurora at full moon

Pic. 12 The aurora visibility just 3 days after full Moon (

Of course, the full Moon can draw out the faint aurora considered i.e. as level IBC2.
The solar position of 11 or even 10,5 degrees below the horizon still enables us to have a good aurora spectacle then. The situation starts to change beyond this point, making the event faint on the brighter side of the sky, whereas the antisolar direction can be still good for enjoying the strong aurora (Pic. 13), although its appearance is getting limited quite quickly, as the directly illuminated part of the stratosphere concerned moves upwards bringing more and more scattered sunlight.

Aurora twilight 9 degrees Spitsbergen

Pic. 13 The aurora borealis appearance above Spitsbergen on March 20, 2015, after sunset, when Sun was about 9 degrees below the horizon. In these conditions, the string aurora concerned as 8 or 9 Kp-index can be visible well on the quite bright sky (György Soponyai/

The event as presented above (Pic. 13) happens quite rarely. We should be aware, that most aurora structures peter out at this moment of nautical twilight. For as much as the standard aurora (with index IBC3) is concerned, we shall expect it disappearance at a solar position about 8 – 8,5 degree below the horizon. It comes at least from my own webcam observations from the Abisko National Park webcam, where the aurora was predominantly gone at the mid-nautical twilight. Regrettably, the scarcity of this data cannot define roughly the moment, at which the aurora is drowned out by the twilight sky. There are 3 reasons behind the insufficiency of this data: lack of good weather between January and late March 2021 – the concerned period of the observation series, not favorable azimuth of webcam bearing, which is north. As a result, twilight encroaches the frame as the day gets longer. Finally, the moment of solar activity falls nearby the minimum, resulting in relatively poor aurora development (Pic. 14, 15).

Aurora at nautical twilight, last moment, Abisko

Pic. 14 Aurora chasing until the last moment when could be detected in the webcam located in the Abisko National Park. The value in the brackets points to the position of the Sun against the horizon in degrees (

Abisko National Park aurora visibility at twilight

Pic. 15 Aurora visibility at twilight in the Abisko National Park on February 16, 2021. The value in the brackets points to the solar position against the horizon in degrees (

As an assumption, I would extend the aurora visibility by at most one degree, although it definitely requires further observations, especially on-site. Even so, it would mean, that aurora becomes invisible for an observer yet during the nautical twilight. Unfortunately, there is no evidence for aurora visibility at civil twilight, which excludes the appearance of this phenomenon along with a total solar eclipse occurring high in the sky.
The aurora occurrence is a very wide topic, which will be definitely discussed here in the future, as it’s not only eclipse-related. I just wanted to bring some general view on the brightness against the twilight sky, which is the pivot thing in terms of the aurora occurrence along with totality. For August 2026, in Russia we could have the situation as per the pattern below (Pic. 16):

Total solar eclipse 2026 in Russia and aurora (northern lights)

Pic. 16 The pattern showing a possibility of aurora visibility at the same moment, when a total solar eclipse occurs. The situation is possible in Northern Russia (Taymyr peninsula), around midnight sun, where: 1 – eclipsed Sun; 2 – lunar shadow extended across the sky; 3 – aurora oval estimated on August 2026; 3a – aurora barely and shortly visible due to still bright sky; 3b – aurora the best and the longest visible south of zenith, where the sky is believed to be the darkest.

Considering the movement of the magnetic pole towards Russia upon 2026 (Pic. 8) we shall expect the aurora oval to be visible just about East and West cardinal points. The best chance to see the aurora is believed to be a bit south of the Zenith, very high above the southern horizon, preferably 75-80 degrees. It would be fantastic, as this section of the sky seems to be the darkest at the moment of totality. The whole situation wouldn’t last for long, and only near the zenith, we could enjoy some faint aurora appearance.

II. TOTAL SOLAR ECLIPSE BELOW THE HORIZON AND NOCTILUCENT CLOUDS (NORTHERN & CENTRAL RUSSIA) – Unlike the aurora, which results from its own light, the noctilucent clouds reflect the sunlight. They are also appreciably lower than the aurora since the first phenomenon can be floated between 80 and even 640km above ground, the second one forms somewhere between 75 and 86km above the ground. These clouds are composed of tiny crystals of water ice, which perfectly reflect the sunlight from the Sun located shallow below the horizon. There are a few theories on how these clouds are produced. The one reasonable explanation says that they are formed with water vapour which comes to the upper atmosphere through gaps and the dust being originated from tiny meteors coming from space. The water vapour is lifted from the troposphere by powerful thunderstorms and the airflow over mountain ranges.  Regardless of it, the moisture of the mesosphere is very little and states about one hundred millionth that of air from the Sahara Desert. These clouds form under very restricted conditions.  They need an environment with a very low density, which is typical for the mesosphere. The temperature must be as low as -120°C or even lower. It happens only during the summertime in the local hemisphere when the mesopause is cooler than during the winter (mesopause anomaly).  It’s driven by the summer-to-winter circulation, which happens in the middle of the atmosphere. In warm months, the polar air close to the ground gets heated and rises upwards. Next, this rising expands, as the atmospheric pressure is lower with the altitude. As a result of warmth, these air masses can reach extremely high altitudes in Earth’s atmosphere and cooling it down adiabatically. When the temperature drops below -120°C it enables the cubic ice crystals to condense around small dust nuclei and form the night-shining clouds. These nuclei are often meteoric debris. Meteors shine at around 100km altitude, which makes its remnants suspended in the upper atmosphere for the period of up to three years (Bone, 2007). During hot summers, the temperature in the upper mesosphere can plunge down even to -210°C. The temperature threshold is usually reached around mid-May in the northern hemisphere. The whole season for noctilucent clouds depends on the weather during the summer period (especially temperature) and lasts upon mid-august on average (reports from north-west Europe) with the peak just after the summer solstice (accordingly between the third week of June and second week of July). Noctilucent clouds have various structures and vary from an hourly to a daily basis because i.e. changes of the gravity waves. These waves create something like a wave-covered surface (covering sometimes several levels) that moves in total usually towards the west direction. Sometimes they can propagate in different directions, disappearing and reappearing or changing the scale (Dalin et al., 2004). Noctilucent clouds feature short and long wavelength structures. The short ones are usually quite unstable in their lifetimes and their instability is very similar to the Kelvin-Helmholtz structure (Fritts, 2014).

Noctilucent clouds structures Yourshire near Pickering

Pic. 17 The typical structure of noctilucent clouds. Near Pickering, Yorkshire, UK.

The life cycle of these structures rarely exceeds 10 minutes. Long wavelengths (between 20 and 70km) are rather stable and can persist even more than an hour. The speed of noctilucent clouds can occasionally reach even 200m/s (Ludlam, 1957). The polar mesospheric clouds structures appear as thin, decayed cirrostratus and cirrus clouds with white or silvery-blue light. A bright observer will notice that visually the polar mesospheric clouds represent 3 sets of tints. Since the very typical one is mentioned above, there are another 2, which are modified by the Earth’s atmosphere.  At the very top of the section, where all noctilucent clouds structures appear, we can spot some reddish tinge. This is the “place” in the mesosphere, where the Sun rises or sets. The mechanism is analogous to sunset saw from the ground.  The rays must come through the thickest atmosphere layer possible, hence the long wavelengths prevail. The same analogy applies to the noctilucent clouds saw just above the horizon. They don’t look bluish at all there. Their color is mostly yellow or even orange. It brings the same effect with the Earth’s atmosphere. The light reflected by them passes through a massive chunk of the atmosphere, so a similar extinction and shift towards longer wavelengths is observed.

Obłoki srebrzyste Szczepańcowa

Pic. 18 The tints of Noctilucent clouds, where: 1reddish tinge corresponding to the sunrise moment at the level of the polar mesospheric cloud deck; 2 – the true color of noctilucent clouds – pale blue; 3 – the true color of noctilucent clouds modified by atmospheric extinction, which shifts it towards red, making a finally yellow-to-orange appearance as moves your sight closer to the horizon. Subcarpathia, Poland.

The polar mesospheric cloud structure can be also shaped by the dissipation of ice in the mesosphere. The ice can form as a single and continuous layer stretching along tens of kilometers. Within these forms, the ice is highly concentrated, which results in higher albedo translated into a significant brightness. A combination of the factors described above makes the polar mesospheric clouds quite elusive throughout the night period. They also change within a wider range of time, covering the whole season or several seasons, which is driven by its subtlety.
Noctilucent clouds are very sensitive to any changes in their environment, which might basically decide about their presence in the sky as well as their structure and brightness. These changes apart from temperature and water vapor might be gravity waves, planetary waves, and even solar activity. Regarding the last one, it was found, that the most intensive noctilucent clouds appearance is characteristic for the lowest solar activity period, presumably because of the generally lower atmospheric temperatures prevailing at these times (Bone, 2007). Another reason behind it might be the ultraviolet radiation from the Sun, which is known to vary cyclically with the solar cycle and peaks during the highest solar activity.  The UV radiation breaks water molecules apart, which reduces water supply to form noctilucent clouds. In turn, they are less bright or less often visible. The newest researches inform about the constantly increasing frequency and intensity of noctilucent clouds, which is probably caused by climate change. It appears to be driven by increasing greenhouse gas concentration in the mesosphere. It has been told that higher methane concentration leads to increment of moisture by producing water vapor when methane breaks down by sunlight in the upper atmosphere. Another greenhouse gas – carbon dioxide radiates the heat towards space and causes cooling of the mesosphere. The result is visible very well by the intensified appearance of polar mesospheric clouds including also its increasing brightness and extending the area and period of visibility.

Noctilucent clouds vs climate change

Pic. 19 The polar mesospheric clouds visibility against climate change throughout recent decades (

Polar mesospheric clouds (Noctilucent clouds) visibility throughout the season vs total solar eclipse 2026

Pic. 20 The noctilucent clouds visibility throughout the season and how it changes in recent years in terms of the day, when 2026 total solar eclipse will occur (

From our point of view important is, that the forthcoming 2026 total solar eclipse falls just above 50 days after the summer solstice, when the probability of polar mesospheric clouds occurrence can be still quite high (Pic. 17). We have on average about 15% of probability, that the eclipsed twilight will coincide with the polar mesospheric clouds occurrence, although the peak of the solar cycle might bring this value further down to about 5% or so. It’s still enough to consider this phenomenon from two points of view – its geometry and brightness.
In terms of noctilucent clouds geometry I mean mainly the level of their deck, which varies between 75 and 85km above ground, making them the highest clouds in the Earth’s atmosphere. I would like to explain their geometry much wider in the future with relation to the whole twilight period. For now, the pattern presented below should be sufficient (Pic. 21).

Noctilucent clouds geometry

Pic. 21 The pattern of the visibility of the noctilucent clouds on the twilight sky (

These clouds remain visible under specific conditions, which come from their optical properties. Admittedly, the finest and thickest NLC structures can be really bright, although they are never bright enough to shine during the daylight. They start to be visible when Sun is at least 4 degrees below the horizon. Thinner polar mesospheric clouds are usually visible upon the end of civil twilight. Predominantly they are visible between 50 and 65 latitudes. They can’t be observed inside the polar circles, because the Sun is never deep enough below the horizon. At the edge of the polar circle, the noctilucent clouds season might be broken up between two smaller periods, as its starts in the mid-may and lasts till mid-august. Therefore, the polar mesospheric clouds are barely visible about 5 weeks before the solstice, as the Sun goes about 4-5degree below the horizon, and they start to be visible again after mid-July. To be more precise, if an observer is located near the edge of the Arctic circle even up to the 71 latitudes (Ludlam, 1957), he is able to watch the polar mesospheric clouds usually after the mid-summer period, somewhere between late July upon the noctilucent clouds disappear completely. The same situation applies to the Antarctic circle in the opposite sequence.
Despite that noctilucent clouds tend to occur in extensive sheets, usually the part of the sky, when we can see it is very restricted to the narrow segment above the horizon. This segment becomes wider, as Sun goes closer to the horizon.
The noctilucent clouds can be visible until Sun is as deep as 16 degrees below the horizon. It’s explained by their altitude, which also determines the zone of visibility (Pic. 22, 23). If the polar mesospheric cloud is visible roughly above your head at the zenith, the other observers can see it in the circle of 800-900 km away (Dietze, 2016). It’s possible because of their strong contrast with the sky, as they reflect a lot of sunshine.

Earth atmosphere, Aurora, NLC

Pic. 22 The simple cross-section through the Earth’s atmosphere depicting the polar mesospheric clouds and aurora altitude compared to the troposphere (Wikimedia/

The altitude of noctilucent clouds compared to the troposphere

Pic. 20 The altitude of noctilucent clouds compared to the troposphere (

As the Sun is closer to the horizon, the segment of the sky, where the noctilucent clouds are visible gets wider. The best pattern is presented below (Pic. 24), where you can clearly see the dependence of the NLC segment of visibility from the solar depression.

NLC visibility against solar depression

Pic. 24 The dependence of noctilucent clouds visibility. The left values represent the maximum altitude of noctilucent clouds, which corresponds to the solar depression angle on the right (

As the Sun goes closer to the horizon, the section of the sky, where the polar mesospheric clouds are visible gets wider. When the Sun is about 8 degrees below the horizon, we have almost half of the sky covered by these clouds. Obviously, we are not exactly sure about the total coverage of the sky by these clouds, because we can see only the visible ones. When Sun reaches 6-degree depression, they cover almost two-thirds of the sky. For 4 degrees, their limit of visibility is pushed further, although at this moment they become too faint for being distinguishable for an observer. Another thing is, that as the sky gets brighter due to lower solar depression, we are successively unable to see the noctilucent clouds towards the solar azimuth (Pic. 25).

Noctilucent clouds vicsibility against solar depression

Pic. 25 Angular elevations of upper and lower borders of the visibility of the noctilucent clouds with relation to the solar azimuth and solar depression. The key moment occurs, when the Sun is about 8 degrees below the horizon. Then, an observer can see the noctilucent clouds near the zenith, but they gradually disappear near the horizon towards the solar azimuth, as it gets brighter (Ludlam, 1957).

The pattern above shows the 12 degrees of solar depression interval, during which the noctilucent clouds can appear anytime in any part of the twilight oval. When Sun is lower than 16 degrees below the horizon, they fade out altogether. On the other hand, predominantly, the polar mesospheric clouds visibility reaches the edge of the civil twilight. However, during spectacular displays it’s not a problem to spot them upon solar depression reaches 4 degrees (watch the video below), or even they can nearly follow the sunrise or sunset. The graph above (Pic. 25) applies rather to the brightest appearance of the noctilucent clouds. The brightness is a key feature from our point of view, as we are considering observing them along with the occurring total solar eclipse in 2026.
The brightness of polar mesospheric clouds marks the basic division between them. It has been classified into 5 levels of illumination (the NLC brightness scale), where the most important is level 5 covering the structures able to illuminate objects noticeably and even casting shadows in extreme cases.
The brightness of noctilucent clouds is predominantly caused by the increase in water vapor concentration and often goes along the lengthening of the NLC season (Klostermeyer, 2002). The brightness of noctilucent clouds is approximately 5-10 times less than the brightness of the diurnal sky (Sharonov, 1965). The brightness of the twilight sky is different and changes dynamically along with solar depression. It’s a nice subject for discussion in the separate article. If the brightest noctilucent clouds fade out at solar azimuth, when Sun is about 8 degrees below the horizon, their illuminance is not bigger than 0.348 Lux. It leads to the conclusion, that in extreme cases, the noctilucent clouds might be brighter than the full Moon. It’s only far-reaching simplification only for the purpose of this writing, at least because of the structure of these clouds. If we are talking about the brightest polar mesospheric clouds possible to spot, we should know, that their brightness is not uniform across the whole sheet. They feature more and less bright structures.
Next to the brightness, the probability of noctilucent clouds occurrence seems to be also very important. Usually, they tend to reach lower latitudes above vast landmasses. It’s predominantly driven by the following factors:
enhanced gravity waves developed from the effective airflow above mountain ranges,
stronger warm air uplift caused by intensive heating of the ground. The ground gets warmer much quicker than a large waterbody
– finally, the human emission, in which the effect, the methane is released to the atmosphere and more water modules is produced in the mesosphere,
Because northern and central Russia is a part of a colossal landmass (Eurasia), the noctilucent clouds occurrence during the 2026 total solar eclipse below the horizon is really likely, especially when we combine it with their season lengthening described above.
This celestial occurrence could look like below (Pic. 26). In addition, an observer would be able to see the solar limb reddening perfectly, just near the umbral edge.

noctilucent clouds and total solar eclipse 2026 below the horizon imagination

Pic. 26 The imagination (photomontage) of the total solar eclipse 2026 below the horizon in accompany with the noctilucent clouds visible somewhere in Northern or Central Russia upon 16 degrees of solar depression. An observer would be able to see the pale blue polar mesospheric clouds sheet turning into the reddish tinge closely to the umbral border, as the limb reddening plays the key role. The sky will be significantly darker inside the umbra with no NLC visible at all.

III. TOTAL SOLAR ECLIPSE BELOW THE HORIZON WITH ACCOMPANY OF BOTH AURORA AND NOCTILUCENT CLOUDS (NORTHERN RUSSIA) – The situation, which can happen, for sure. If we are at high latitudes, we can experience sometimes the northern lights and noctilucent clouds at once (Pic. 27).

Aurora and noctilucent clouds

Pic. 27 A display of Northern Lights along with noctilucent clouds on the northern horizon at right being lit by the Sun. Perpetual twilight colors the sky blue and the horizon a deep orange. A remarkable display of sky colours (Alan Dyer/

The occurrence of both phenomena is a fantastic spectacle. It can be an extremely unique celestial event, when it combined with the total solar eclipse below the horizon, as per the pattern below (Pic. 28).

Aurora (Northern lights), noctilucent clouds (polar mesospheric clouds) and total solar eclipse below the horizon in Russia august 2026 pattern

Pic. 28 The pattern of solar eclipse below the horizon at 9 degrees of solar depression, when both aurora and noctilucent clouds are visible, where: Z – Zenith; EWN – cardinal points; 1a – lunar shadow within illuminated ozonosphere; 1b – lunar shadow beyond the Earth’s shadow (double solar eclipse); 2 – Earth’s ozonosphere and lower atmosphere inside the Earth’s shadow, geometry appropriate for solar position preferably 9 degrees below the horizon, 3 – Earth’s ozonosphere and lower atmosphere still illuminated by Sun (crescent sun); 4a – noctilucent clouds shining in pale blue; 4b – noctilucent clouds affected by the shift towards red caused by solar limb reddening; 5 – the aurora appearance optionally near the zenith.

solar eclipse below the horizon 2026 Russia simulation with nlc and aurora

Pic. 29 The visualization (photomontage) depicting the occurrence of total solar eclipse below the horizon on August 2026 in Russia along with the noctilucent clouds and northern lights.

The same as described above, the noctilucent clouds should be completely gone at the time, when the umbra emerges in the twilight sky. Unlike the horizontal solar eclipse, as concerned above (Pic. 16), the probability of aurora display is much higher, because the twilight sky is definitely not as bright as during the day or golden hour period. In turn, we shall expect the spectacular combination of clear northern lights filling up the “space” after polar mesospheric clouds shaded by Moon’s shadow for a while or appearing near zenith when we are located further north. There is also a likelihood, that the noctilucent clouds would extend their visibility even beyond sunset due to totality conditions. Considering the illuminance conditions under eclipsed Sun shining at the horizon, as similar to nearly nautical twilight with 8 degrees of solar depression, the polar mesospheric clouds could be visible across the entire sky wherever illuminated by crescent Sun. On the other hand, I can’t assure, that this situation can happen at all because the brightness of noctilucent clouds will be accordingly lower because of the high eclipse magnitude. However, if we assume, that the given NLC structure can be visible even from 800km, where the eclipse magnitude is significantly lower, this situation can’t be excluded completely. A quite good approach confirming or rejecting this theory can be the NLC investigation under annular eclipse conditions in June 2021 in Minnesota, US, where the ring of fire will be about 2 – 5 degrees below the horizon at the greatest phase.

IV. LIGHT SCATTERING IN THE ATMOSPHERE INSIDE THE UMBRA PERFECTLY SEEN ON WHITE SURFACE (GREENLAND, ICELAND) – it’s going to be the best occasion to see how the light is reflected from the surface, and what coloration of scattered light takes hold throughout the entire period of totality. There are no better conditions to observe it than a huge white or almost white surface which is i.e. the glacier body. The Greenland Ice sheet covers roughly 79% of Greenland’s surface. It does look amazing, even when watching it from cruising altitude you are unable to determine, where is its end (Pic. 30).

Greenland Ice Sheet Norwegian OSL-OAK

Pic. 30 The Greenland Ice Sheet north of Watkins Range, which will fall within the 2026 path of totality. The view from cruising altitude, OSL-OAK.

The opportunity for this scientific optical experiment will be undeniably the best unlike most of the eclipses, where only white sheets are used for this purpose.  The last occasion for observation such this was at Spitsbergen in 2015, which in winter conditions resembles the scenery of Greenland at some point (Pic. 31).

Svalbard 2015 total solar eclipse light scattering

Pic. 31 The light scattering on the white, snowy surface at Spitsbergen n March 20, 2015 (Arne Danielsen/ Click to enlarge.

Another chance comes this year on December 4, when totality will occur in northern Antarctica.

V. LARGE SCALE SHADOW BANDS CHASING (GREENLAND & CRUISING ALTITUDE) – The Greenland Ice Sheet will be also the best place for the shadow bands study, as they are the clearest visible on a white surface. These wavy and alternating white and dark lines can be seen immediately before and after the totality. There are at least a few theories, what exactly causes shadow bands. Before the eclipse, they pass on the ground towards the direction, in which the umbra is traveling. After totality, the bands are often seen spreading at an angle to the eclipse’s course. The main theories explaining fairly the shadow bands talk about light diffraction, atmospheric scintillation, and infrasound. The light diffraction can be explained by the light shining by a thin solar crescent only. In this situation, the sunlight reaches a particular place on Earth’s surface by a variety of paths, where each of them is bent under different angles when passing through the atmosphere. Thus, in some places, the light waves are reinforced bringing the higher light level, whereas in other places the light level is reduced as the waves cancel each other. In turn, we can see a ragged banded pattern of light.
Another theory is based on infrasound – the sound which is too low to be heard by the human ear. This sound is believed to be caused by the sudden temperature changes in the Earth’s atmosphere driven by the Sun’s disappearance. This rapid cooling of the ear triggers changes in the pressure, and next the potential energy associated with this pressure difference escapes as high-intensive infrasound. These sound pulses are created continuously along with the “shock front” moving ahead of the eclipse itself. It creates a pattern of peaks and troughs in the atmosphere causing changes in the speed and direction of the light waves, which can be observed as the shadow bands on the ground.
Finally, the atmospheric scintillation is an analog phenomenon, as we can observe for distant point light sources like stars, which light beam is refracted on its way through the Earth’s atmosphere. On this basis also shadow bands can be produced. Atmospheric scintillation is a product of air turbulence caused by rapid changes in temperature and pressure. Since these disturbances in a transparent medium refract light waves, the disturbances can effectively cast shadows. If the bright source is thin and elongated, the shadows which are cast will generally be aligned parallel to the orientation of the source. Thus, when the background light source is the bright thin crescent of the Sun before and after totality, the shadow cast by Earth’s atmosphere will scintillate and appear as the bright and dark bands on the ground, which are parallel to the crescent (Madhani, 2020).
The shadow bands can be observed on large scale for instance from the plane flying above plain-coloured surface, which is the Greenland Ice Sheet. Shadow bands were observed even higher, about 25km above the ground during the 2017 total solar eclipse in Tennessee (Madhani, 2020). If you want to learn more about the mechanism of shadow bands, this link is the best for understanding how it works.

Possibility of watching shadow bands from the plane

Pic. 32 The possibility of watching shadow bands from the plane just before totality occurs. The best occasion will be above the Greenland ice sheet when the weather is clear. The footage above shows the analog situation as appeared on the uniform cloud deck above North Atlantic Ocean on March 20, 2015. The question mark indicates the moment when shadow bands could be possible to spot (Martin Junius/

VI. ENHANCED CONTRAST TRIANGLE (UNITED KINGDOM & REPUBLIC OF IRELAND) – this intriguing optical illusion, described here,  will be definitely enhanced, although not necessarily by the solar crescent, because during the partial solar eclipse, the level of brightness changes uniformly in all directions. The matter applies to the southwest shores of Great Britain (especially Cornwall) and Ireland (especially Beara, Iverag, and Dingle Penninsula), where the partial phase of the eclipse will be the biggest. It will be accordingly almost 96% obscuration for the Land’s End in Cornwall and near 98% obscuration at Dursey Island, just outside of the Beara Penninsula (Pic. 33).

Deep partial solar eclipse UK and Ireland 2026

Pic. 33 The deep phase of the partial solar eclipse at south-west shores of the UK and Rep. of Ireland.  The biggest magnitude will occur at Skellig Islands (Skellig Lighthouse) outside of the Iverag peninsula. In the UK, the place with the greatest magnitude will be the Isles of Scilly(

Moving a bit outside of the mainland, we shall expect the greatest magnitude accordingly at Skelling Islands in Ireland and Isles of Scilly in England.
An observer at Irish shore will watch the greatest partial eclipse, just about 230km away from the shadow. Therefore, it’s possible to see the coincidence of the contrast triangle phenomenon with umbral column beyond (Pic. 34), taking into account, that the shadow can be noticeable even from 250km. We should expect there the dark triangle standing at the horizon, straight above the solar glitter, which would tend to faint as moving away from the sea bank. Beyond this triangle, an observer would be able to spot moving umbra, displayed as significant greyish or bluish sky extended much further than the bounds of this optical illusion, quite similar to the grayish shadow cone observed immediately before and after totality, when watching it at the similar azimuth, where the Sun is located.

Contrast triangle and shadow column 2026 eclipse Ireland

Pic. 34 The visualization of the contrast triangle coincidence with the fleeting shadow cone at about 230km distance. It’s possible to see from south-westernmost Ireland on August 12, 2026, late afternoon, where: 1 – crescent Sun with about 0.98 eclipse magnitude; 2 – the bounds of a distant umbra; 3 – the contrast triangle phenomenon enhanced by a darkening scene towards the path of totality; 4 – Sun’s glitter on the sea surface, fading out slightly towards the full eclipse region.

If the umbra wouldn’t be visible because of atmospheric conditions (mist or haze), then the contrast triangle would appear in a seriously darker sky. A bit different situation should be expected in the southwesternmost part of the UK, where the mainland will be about 420km away from the umbral path. There is rather no chance to spot the column of shadow, but the contrast triangle will be accompanied by a definitely darker sky towards the solar azimuth. In both cases, this assumption is really possible, as the greatest eclipse will occur in the late afternoon hours.

VII SUN’S GLITTER DISAPPEARANCE (SPAIN) – Another fantastic optical phenomenon possible to spot immediately before and after totality, when the glitter reappears again. As long as direct solar beams hit the water surface, an observer can see their reflection at the angle of incidence. A full explanation of this phenomenon you can find in this article. When totality approaches and an observer is high enough above sea level, then he can see how this solar glitter is getting shorter dramatically, until completely disappear inside the umbra. Next, after the human eye adaptation and light transition moment, he can see the same glitter, but as the effect of shining the solar corona, which as has been told is as bright as the full Moon. When the umbra moves away, this dimmer glitter is successively superseded by the solar one, which emerges straight after the shadow (Pic. 35).

Suns glitter 2019 total solar eclipse in Chile

Pic. 35 The solar glitter disappearance and reapperrance (displayed in reverse sequence) during 2019 total solar eclipse in Chile, where: 1 – Sun’s glitter; 2 – solar corona’s glitter.
We can observe the phenomena like this mostly when Sun is low enough above the horizon, where most of the light is reflected from the waterbody instead of diffracted inside this medium (Fresnel equation). Moreover, the elevated position gives an opportunity to watch how this glitter yelds the umbra and other way round at the end of the eclipse ( Click to enlarge.

Another thing, which can be spotted, when we are significantly elevated above the sea body is the perspective effect. Both Sun’s glitter disappearing and reappearing increases its pace, from the observer’s point of view. The light transition phenomenon also plays an important role here. Before the totality begins, we can see how the Sun’s glitter ceases abruptly before the dark area beyond. When eclipse is about to finish, apart from the bright Sun’s glitter reappearing far away, we can see also the solar corona light reflected at our plane of incidence. Another, very important factor is our height above sea level. As we are located higher, then this whole phenomenon is better seen and a bit lengthened, because we have longer line of sight. With relation to 2026 total solar eclipse, undeniably the best place to see it will be Spain. There are at least 2 spots considered (Pic. 36), where the one is the Vixia da Herbeira hill – a fantastic viewpoint rising over 600 meters above sea level in the A Coruna province and Sierra de Tramuntana at Mallorca, where you can see the Mediterranean Sea surface from the highest mountain – Puig Major, rising 1436 meters above sea level as well as many other peaks reaching around 1000m.a.s.l. In both places you can get about 1m40s of totality.

Solar glitter locations 2026 total solar eclipse Spain

Pic. 36 The best locations for admiring the solar glitter disappearance by the total solar eclipse in 2026 (

VIII. HORIZONTAL VISIBILITY EXTENSION (SPAIN) – staying by Sierra de Tramuntana mountain range at Mallorca island, we should mention about one interesting fact. The Puig d’en Galieu is the peak, from where the World’s longest distance within one country has been captured. It’s roughly 324km between this peak and Pic de Saloria in the Pyrenees. The Puig d’en Galieu towers above the Lluc sanctuary.

Pyrenees from Mallorca

Pic. 37 Pyrenees mountain range saw from Sierra de Tramuntana. This is so far the longest distance observation within one country – 324km ( See an original image here.

Because the direct light scattering stops when the air is shaded totally, the horizontal visibility is extended. There are 2 factors, which determine this situation. The first one is the significant reduction of light scattering at the air molecules and haze particles, in which effect the light reflected from distant features is not as much interfered. The second reason is the contrast, which is significantly higher between shaded objects and sky just above the horizon, illuminated by the sunlight outside of the umbra. In the case concerned, only the first factor would work, as the Pyrenees won’t experience the totality.  Nevertheless, the eclipse situation might be helpful for someone, who wants to repeat this long-distance observation record.

IX. CRESCENT SUNSET BEHIND HIGH MOUNTAIN RANGES (EUROPE) – the rare event, when Sun goes under horizon not as a disk, but as a quite thin crescent. The 2026 solar eclipse will have a significant impact on the evening time, as virtually everywhere in Europe, the obscuration will be not lower than 80%. On top of that, the moment of greatest eclipse will predominantly fall near sunset or just after the sunset. It means, that the moment, when Sun goes under the horizon will be so spectacular, especially in the regions with nice mountainous views on the horizon. On August 12, 2026, some Europeans will be fortunate to witness one of the most spectacular sunsets ever, by seeing the crescent Sun plunging beyond high mountain ranges and some most renowned peaks (Pic. 38, 39).

Crescent sunset 2026 solar eclipse Europe Corsica, Alps, Tatras

Crescent sunset 2026 solar eclipse Europe Corsica, Alps, Tatras

Pic. 38, 39 The simulation of the eclipsed sunset above popular mountain peaks in Europe, where: 1 – view from Makovica in Slanske Hills at High Tatras (Slovakia); 2 – View from Kordazeva Glava – Petzen, Karawanks (Slovenian & Austrian border); 3 – view from Piacenza towards Graian Alps (Italy); 4 – View from Aleria village at Corsican Mountains (France); 39 – the map with an arrow pointing the crescent sunset azimuth ( Click to enlarge.

There are only 4 examples presented above, but the same situation will apply to the Sierra Nevada and others located in Europe. An observer will see the setting eclipsed Sun. The most spectacular crescent is believed to be observed in northern Italy, where the greatest phase will coincide with the sunset.

X. THE PERSEID METEOR MAXIMUM – August 12 is usually the peak of the Perseid meteor shower, which is the remnant of the Swift-Tuttle comet returning near the Sun every 133 years. The most intensive shower can bring even 300 meteors per hour like happened in 1993, a year after the comet recently passed the inner Solar System. In the situation of the total solar eclipse, the most important is the possibility of occurrence the brightest fireballs with apparent magnitude -3Mag and higher. The thing, which can make the meteor shower brighter is the orbital resonance in the Solar System, which in the Perseid meteoroid stream involves three bodies: the meteoroid particle, Jupiter, and Saturn (Sekhar, Asher, Vaubaillon, 2016). We could recently see the intense Perseid showers in the early 1990s, and the next situation like this is going to happen around 2111, what corresponds more or less to one orbital period of the Swift-Tuttle comet, although it still requires further research. Despite lack of this resonance in 2026, we will still enjoy a good meteor shower, knowing that the Perseids are one of the most plentiful showers with an average of 50-100 meteors per hour, threading its way about 2 meteors during the 2026 totality. The best chance to spot the Perseids at the same time, when a total solar eclipse is occurring will have observers at the northern part of the path, where the Perseid constellation remains above the horizon throughout the entire day. The Perseid constellation is the section of the sky, where the Perseid radiant is observed – the point in the sky, from which this meteor shower comes (Pic. 40).

The Perseid and delta aquarid radiant EarthSky org

Pic. 40 The meteor showers active around August 12 and their radiant points in the sky (

It’s good, when the radiant is above the horizon, then we have a better chance to enjoy the shower, however, we shouldn’t look directly into the radiant point itself. The best way is to chase the meteors and fireballs about one-third of the sky down and away from it. In this case, we might have also an opportunity to spot some unusually bright Perseid meteor somewhere within the eclipse path in Spain, where the Perseid constellation will be just beneath the horizon at the time of the greatest eclipse (Pic. 41).

Total solar eclipse 2026 Spain and erseid fireballl

Pic. 41 The visualization of the Perseid fireball possible to chase during total solar eclipse 2026 in Spain on August 12, when usually the Perseid meteor shower peak occurs (photomontage based at the 2019 total solar eclipse in Chile and Meteor image/

A tad better conditions will occur in Italy, Tunisia, and Malta, where the totality will fall beneath the horizon around the end of civil twilight. An observer should spot not only the fireballs but also another, less bright meteors fleeting across the sky. The Perseus constellation should be rising from that locations during the eclipse. The Perseids in general tend to be bright, so it shouldn’t be a problem to spot at least one of them during the eclipse, especially when it occurs low above the horizon. During the evening hours, when Sun is about to set, the sky is usually a bit darker than during the afternoon. Any additional loss of brightness increases the chance to see an event such as this. In the areas located at the extension of the totality path, the view of the Perseid shower is more likely, as the double darkened sky (by the twilight and lunar shadow) gives the way for more meteor light to get through and be visible for an observer. As a result, we are able to see the fleeting meteors more often. The frequency of 50-100 meteors per hour refers to the nighttime conditions, where the sky is dark. Even the moonlight can reduce the number of meteors visible. The probability of spotting the fireball during the total solar eclipse is really low then, although not impossible. What is comforting, that along with Perseids the Delta Aquariids appear at the same time in the sky. Their peak of activity falls on July 28, but they can be still observed till August 23. Their radiant is located on the other side of the sky (Pic. 40) and will be just below the horizon at the time of the greatest eclipse. The same as previously, for areas, where this totality occurring below the horizon, the chances for chasing the meteors will be slightly bigger.

2026 total solar eclipse below the horizon and Perseid and Delta Aquarids meteor showers

Pic. 42 The pattern which displays the situation during total solar eclipse below the horizon with respect to active meteor showers and their radiants marked as stars, where:  NESW – cardinal points; Z – zenith; O – the observer’s place; 1 – umbra extended across the sky; 2 – Earth’s shadow shaded additionally by the umbra (situation described here); 3 – the Earth’s shadow outside of the umbra; 4 – the Belt of Venus; 5 – the Perseid’s radiant; 5A – possible Perseid meteor appearance; 6 – the radiant of Delta Aquariids; 6A – possible Delta Aquariids meteor appearance. The pattern is valid for Trapani (Sicily, Italy) where the greatest eclipse will occur at 5-degree solar depression.

XI. TOTAL SOLAR ECLIPSE BELOW THE HORIZON AND ZODIACAL LIGHT (ITALY, ALGERIA, TUNISIA, MALTA, GREECE) – This option has been already discussed in terms of total solar eclipse below the horizon of June 30, 1992 (Guliaev, 1992). Because it was only the proposal, we don’t have visual proof of the observation such as this. The good occasion it’s going to happen in August 2026 in the Mediterranean region, where the totality will fall predominantly below the horizon. The zodiacal light is visible as a softly bright cone of white light, which extends from where the Sun is located below the horizon outward and upwards along the ecliptic. The brightness of zodiacal light is similar to the brightness of the Milky Way, so these 2 objects in the sky can be sometimes mistaken.  However, during the best conditions, the zodiacal light can be significantly brighter than Milky Way. The zodiacal light is produced by the sunlight scattered at thin dust particles from the inner Solar System.  A part of this dust is thought to be leftover after all the planets have been created about 4.5 billion years ago. The dimension of these dust particles reaches usually 0.1mm, and not as much as 0.3mm. They are probably within a few miles distance from each other. Between them can be some another, meter-sized bodies. All of them feature the biggest density around the Sun and extend outward beyond the orbit of Mars. Another part of this dust is occasionally originated from comets or rare collisions of asteroids between Mars and Jupiter. The size of this dust is not always the same. The probability of collisions between each other or space weathering makes their dimensions smaller. If it falls beneath 10 micrometers, the grain is removed from the inner Solar System by solar radiation pressure.
The brightest zodiacal light always appears in the immediate vicinity of the Sun. Hence the best conditions to see it occur shortly before dawn or after dusk. Important is also the season when the zodiacal light can be observed successfully. It’s usually the moment near the equinox when the ecliptic is the most straight-up against the horizon. At the vernal equinox, the best chance to see this cone of eery light is after dusk, because the ecliptic rises higher against the celestial equator and consequently higher above the western horizon making it more intensive at once. At the autumn equinox, the situation is opposite, and the best zodiacal light is visible before dawn. It applies to the northern hemisphere, where the 2026 total solar eclipse will happen. The southern hemisphere is exactly upside down. Unfortunately, the 2026 solar eclipse conditions won’t be as much favorable as considered, because the eclipse will occur near sunset when the ecliptic will be more parallel. However, a quite low latitude might be helpful and will allow observers to spot this hazy pyramid.
The zodiacal light is also called false dawn or false dusk, because of the significant amount of light visible just before or after the twilight occurrence. This situation is driven by forward sunlight scattering on the dust particles described above. In practice, the zodiacal light extends much further away from the Sun, although is fainter. In theory, an observer could see a slightly illuminated band of dust across the entire sky, which marks the same path, as the Sun follows during the day. Next, this faint band of dust leads to Gegenschein, a faintly bright spot in the night sky, marking roughly the antisolar point. This dust band near Gegenshein scatters light backward, which makes its intensity significantly reduced and not as obvious to spot as zodiacal light near the solar azimuth. The zodiacal light, leading next through the dusty band to Gegenschein (or counterglow) is called the zodiacal band.
The zodiacal light can be followed visually from about 22-25 to 90 degrees away from the Sun, but along the ecliptic. It can be considered as the F-corona of the Sun, which is created by sunlight bouncing off the interplanetary dust.
As it has been told earlier, the zodiacal light can be considerably brighter than Milky Way under good conditions. The zodiacal light is always the broadest and brightest near the Sun. Unfortunately, because of the light scattering in Earth’s atmosphere, we can’t see it until the astronomical twilight. We know, that the brightness of zodiacal light at 30 degrees away from the Sun is about 2330 sVis, which corresponds to 0.0016077 Nits and 0.005050734243 Lux. I’ve explained this conversion earlier in this article. The brightness of about 0.005 Lux means, that in the best conditions possible, the zodiacal light should be detectable yet at the end of the nautical dusk. An observer theoretically could see this hazy triangle even more intensive when moves its sight closer to the Sun. The problem is the Earth’s atmosphere, which scatters the sunlight stronger in our point of view. Even if the zodiacal light can be detectable at the beginning of astronomical twilight it won’t look bright, because it will be faded out by the still bright sky. Considering outlook at 30 degrees from the Sun, we effectively get it only 12 degrees above the horizon at the edge of astronomical twilight. Moving our sight further down, this phenomenon should look brighter, but everything depends on the atmospheric extinction, which can make it fainter in appearance. Anyway, the zodiacal light at this angular distance from Sun appears to be about 4x brighter than Milky Way at its equator. At the angular distance of 8 degrees from the Sun, the zodiacal light can be 25 times as large as at the distance of 37 degrees (Fesenkov, 1961). There are quite a lot of images of zodiacal light under astronomical twilight conditions (Pic. 43, 44) when it is distinguishable enough.

Three bands of light Milky Way Zodiacal light and astronomical twilight

Pic. 42 The “Three bands of light” image presenting the Milky Way, zodiacal light, and astronomical twilight glow. The image has been captured probably when Sun was about 16 degrees below the horizon. At this time the astronomical twilight glow is faint enough to yield the bright zodiacal light appearance (Babak Tafreshi/

Due to its significant brightness comparing to the night sky, the zodiacal light is one of the benchmarks for the Bortle scale. It’s usually visible up to the 5th class of this scale, which corresponds to rural areas. Everywhere, where the sky is completely free of light pollution, the zodiacal light can even cast the shadow. Not to mention, that in conditions such as these, this faint light band can stretch from one horizon to the opposite one. When we look at zodiacal light about 60 degrees from the Sun, then its brightness can be comparable with the brightest parts of the Milky Way. The faintest appearance of the zodiacal band is usually around 140-160 degrees from the Sun with the sky surface brightness about 22,2 mag/arcsec2.
Unfortunately, the very brightest part of zodiacal light can be never seen from Earth, because of the aforementioned illuminated atmosphere. The total solar eclipse below the horizon can significantly facilitate the observation of inner F-corona, at least in a theoretical sense. The reason behind it is, that the sky surface brightness doesn’t increase as fast towards the horizon as under non-eclipse conditions. The dust lying closer to the Sun scatters the light more intensely and presumably can surpass the brightness of the eclipsed sky. There are some reports of the zodiacal light observation by the eclipse conditions even when the Sun was high above the horizon. For example, in June 1936 and July 1878, the “beam of light inclined at an angle of 45 degrees” has been reported and it was as wide as Sun (Smiley, 1938). The view could be very similar to early astronomical dusk. However nowadays, when a lot of planes traverse the upper troposphere from one side of the globe to another, we should also consider the possibility of observing the zodiacal light from the cruising altitude. At about 10km altitude, we can see the zodiacal light in the vicinity of eclipsed Sun (Rense, Jackson, Todd, 1953), because the luminance of the background sky is reduced with the sufficient rise of the observer (Fesenkov, 1961).
The conditions on August 12, 2026, won’t be the best, but they might be still favorable to watch or at least detect the zodiacal light at the fully eclipsed sky, taking into account that the solar eclipse in Spain will occur just before set when the sky is less bright than during the afternoon. It’s worth considering watching the eclipse impact below the horizon, not necessarily within the total path but also outside. In both cases, the twilight will be enhanced. Since the sky brightness inside the umbra at daylight conditions is equal to the end of civil twilight, we should expect the nautical twilight conditions somewhere within the extended path of totality at solar depression about 6 degrees or even less. This configuration would make the zodiacal light visible even from Sicily in Italy at the greatest eclipse phase below the horizon. An observation such as this can be tested also for other eclipse locations with smaller solar depression.

Solar eclipse below the horizon and zodiacal light wisualization

Pic. 43 The visualization of zodiacal light visibility when total solar eclipse below the horizon occurs. Image modified from 2010 total solar eclipse in Argentina (Lukas Gornisiewicz & David Makepiece/ and zodiacal light captured above Tenerife (

XII. ACCELERATED AND DISTURBED TWILIGHT (CENTRAL AND SOUTH EUROPE, NORTH AFRICA) – will be undeniably the most visible eclipse impact on the Earth’s atmosphere both in umbral and prenumbral area. In Europe there is no place with obscuration lower than 79,5%, so anyone should notice, that twilight will be quite weird. Depending on the location against the terminator line at the greatest eclipse, some of you might see accelerated twilight, which next will tend to be flattened for a while. A similar phenomenon has been observed recently in Namibia, where the greatest eclipse occurred for solar depression between 2 and 14 degrees (2-10 degrees recorded by webcams). According to these studies, the twilight has been accelerated by 2 degrees on average, which corresponds to the end of civil twilight at 4 degrees of solar depression instead of 6.  The dusk was quite eerie, making the scene darker than usually (Pic. 44).

 Namib Desert Wegkruip twilight eclipse 2020

Pic. 44 The same moment of twilight captured by Namib Desert Wegkruip webcam during the partial solar eclipse and non-eclipse conditions a day after. We can see the significant darkness of the horizon and red shift on the sky (

The eclipse impact on twilight across Europe and North Africa, where the greatest phase is deep enough, will be significantly visible by darkening and slight reddening of the sky. Therefore, the Belt of Venus appearance can be interesting, because of enhancing the reddish tinge. The acceleration of dusk by 2 degrees will definitely bring forward the visibility of stars and other celestial objects, which appear after sunset accordingly to their brightness. It applies also to zodiacal light, which conditions to observe will be better as moves southwards from the extended path of totality.  It will be definitely an unusual moment for some good celestial observations of the sky section being closer to the Sun. The eclipse twilight should feature two separate moments of the same sky brightness when the second one will follow after the greatest phase of the eclipse. The prenumbral impact should be visible relatively long after the eclipse because of a proportionally smaller amount of light scattered in the atmosphere, which has been observed recently in Namibia.

          3. SUMMARY

This long article presents the uniqueness of the 2026 total solar eclipse, which will occur mostly in Europe. This anotherness arises out of the eclipse geometry, which is somewhat typical for each saros when the absolute Gamma value is close to 1. As a result, the lunar shadow is not evenly spaced across the Earth’s surface, making some big part of the planet seriously affected by penumbra near the terminator line. This influence can be expressed mostly as disturbed twilight period, which appears to be the widest and most common phenomenon to observe on the August 12 evening. The brief explanation at the top is helpful with understanding the geometry of the eclipse such as this in 2026. The specificity of this solar eclipse implies a few rare optical phenomena, which can happen at the same time. Some of them, like the accelerated twilight, are sure, but others are only probable. Their optical properties define the various degree of probability of their occurrence along with the greatest phase of the solar eclipse. In fact, the number of visualizations used here leads to the question about their credibility. Are they extremely rare enough, because no one captured them in modern history or maybe there is no chance to see them in a configuration such as this?  I think, the best answer to this question will come at the eclipse day for people, who will be fortunate to be in the locations considered here. Our goal for the forthcoming years is to raise awareness of the beauty and uniqueness of this eclipse with its extension below the horizon too.
The best conclusion of this article is an interactive map including all the phenomena concerned. You can enter the link below, click any of the items and see the short description, which will be probably developed further (Pic. 45).

2026 total solar eclipse interactive map

Pic. 45 The simple interactive map of the 2026 total solar eclipse including all phenomena described in the article (Google MyMaps). Click on the link to open the full map.

The map includes a standard .kml file derived from Xavier Jubier’s eclipse page with all interesting things, which are more or less plausible to observe both by the eclipse chasers and casual people, inhabitants of some area. The Mediterranean region is really potential with the population watching the evening sky on August 12 even accidentally. Our role is to make them aware of this moment, which in my opinion cannot be missed out. The multitude of references and links in this article indicates somewhat further areas of study at the various astronomical and meteorological phenomena with relation to optics of Earth’s atmosphere. So far it should be clear enough for everyone to understanding the importance of the 2026 solar eclipse.


Mariusz Krukar


  1. Baker D.J., 1974, Rayleigh, the Unit for Light Radiance, (in:) Applied Optics, v.13 i. 9, p.2160-2163.
  2. Berger U., Baumgarten G., 2018, On the Anthropogenic Impact on Long‐Term Evolution of Noctilucent Clouds, (in:) Geophysical Research Letters, vol. 45, issue. 13, p.6681-6689
  3. Bone N., 1999, Observing Meteors, Comets, Supernovae and other Transient Phenomena, Springer-Verlag, London
  4. Bone N., 2007, Aurora – observing and recording nature’s spectacular light show, Patrick Moore’s Practical Astronomy Series, Springer, New York
  5. Chamberlain J.W., 1995, The Rayleigh: A Photometric Unit for the Aurora and Airglow, (in:) Physics of the Aurora and Airglow, Volume 41, American Geophysical Union
  6. Craig R.A., 1965, The upper atmosphere. Meteorology and physics, Academic Press, New York, and London
  7. Dalin P., Et al., 2004, A case study of gravity waves in noctilucent cloud, (in:) Annales Geophysicae, vol. 22, p.1875-1884
  8. Davis T.N., Deehr C.S., Leinbach H., 1960, An evaluation of auroral all-sky cameras observation, (in:) geophysical Institute of Alaska, Scientific report no 5.
  9. Dietze G., 2016, Zones of the visibility of a noctilucent cloud, (in:) Tellus, v.21
  10. Dixon F.E., 1939, A 27.3‐day period in the aurora borealis, (in:) Terrestrial magnetism and atmospheric electricity, vol. 44 issue 3.
  11. Ebihara Y., et al., 2017, Possible Cause of Extremely Bright Aurora Witnessed in East Asia on 17 September 1770, (in:) Space Weather, vol. 15, i. 10, p. 1373 – 1382
  12. Espenak F., Meeus J., 2006, Five Millennium Canon of Solar Eclipses: -1999 to +3000 (2000 BCE to 3000 CE), NASA Tech. Pub. 2006-214141, NASA Goddard Space Flight Center, Greenbelt, Maryland
  13. Fesenkov V.G., 1961, The Conditions of Observation of the Zodiacal Light During a Solar Eclipse, Office of Aerospace Research, United States Air Force.
  14. Green J.L., et al., 2006, Eyewitness reports of the great auroral storm of 1859, (in:) Advances in Space Research v.38 p.145 – 154.
  15. Guliaev R.A., 1992, On a possible use of total solar eclipse below the horizon for observations of the inner zodiacal light (as applied to the eclipse of 30 June, 1992), (in:) Solar Physics, vol. 138, p.209-211
  16. Kimura H., Mann I., 1998, Brightness of the solar F-corona, (in:) Earth Planets Space, 50, p.493–499
  17. Klostermeyer J., 2002, Noctilucent clouds getting brighter, (in:)Journal of Geophysical Research, vol. 107, i. D14
  18. Kuliman M., et al., 2017, Exploring noctilucent cloud variability using the nudged and extended version of the Canadian Middle Atmosphere Model, (in:) , Journal of Atmospheric and Solar-Terrestrial Physics, vol. 164, p.276-288.
  19. Ludlam F.H., 1957, Noctilucent Clouds, (in:) Tellus, vol. 9
  20. Madhani J.P., et al., 2020, Observation of Eclipse Shadow Bands Using High Altitude Balloon and Ground-Based Photodiode Arrays, (in:) Journal of Atmospheric and Solar-Terrestrial Physics, vol. 211
  21. Meeus J., Grosjean C.C., Vanderleen W., 1966, Canon of Solar Eclipses, Pergamon Press, Oxford, United Kingdom
  22. Mieghem J.V., 1961, Physics of the aurora and airglow, Academic Press, New York & London
  23. Omholt A., 1971, The optical aurora, Springer-Verlag Berlin, Heidelberg, New York
  24. Proctor R.A., 1871, Notes on the Solar Corona and the Zodiacal Light; with suggestions respecting Observations to be made on the Total Solar Eclipse of December 24, 1870, (in:) Monthly Notices of the Royal Astronomical Society, vol. 30, p.138
  25. Rense A., Jackson J. M., Todd B., 1953, Measurements of the inner zodiacal light during the total solar eclipse of February 25, 1952, (in:) Journal of Geophysical Research, vol. 58, i. 3, p. 369-376
  26. Romick G.J., Belon A.E., 1967, The spatial variation of aurora luminosity, (in:) Planetary and Space Science 15(3).
  27. Russel M.J., et al., 2014, Analysis of northern midlatitude noctilucent cloud occurrences using satellite data and modeling, (in:) Journal of Geophysic Research Atmospheres, vol. 119, i. 6
  28. Sekhar A., Asher D., Vaubaillon J., 2016, Three-body resonance in meteoroid streams, (in:) Earth and Planetary Astrophysics
  29. Sharonow V.V., 1965, Climatology of Noctilucent Clouds According to Observations Performed During the Igy, Meteorologicheskye Issledovaniya, Moscow
  30. Shaw A.J., et al., 2009, Optical aurora detectors: using natural optics
    to motivate education and outreach, (in:) Education and Training in Optics and Photonics 2009, St. Asaph, North Wales United Kingdom
  31. Simmons D.A.R., 1998, A classification of auroral types (in:) Journal of the British Astronomical Association, vol.108, no.5, p.247-257
  32. Smiley C.H., 1938, The Zodiacal Light at a Total Solar Eclipse, (in:) Nature, 141, p. 121-122
  33. Thomas G.E., McPeters R., Jensen E.J., 1991, Satellite observations of polar mesospheric clouds by the solar backscattered ultraviolet spectral radiometer: Evidence of a solar cycle dependence, (in:) Journal of Geophysical Research Atmospheres, vol. 96, issue D1, p.927 – 939.
  34. Yahnin A.G., 1997, Magnetospheric source region of discrete auroras inferred from their relationship with isotropy boundaries of energetic particles, (in:) Ann. Geophys., 15, 943–958
  35. Van den Bergh G., 1955, Periodicity and Variation of Solar (and Lunar) Eclipses, Tjeenk Willink, and Haarlem, Netherland
  36. Vats H.O., Bagare S.P., Bhandari S.M., 2003, Formation and Observations of Shadow Bands During the Total Solar Eclipse of November 23, 2003 Near Maitri, Antarctic, (in:)
    Advances in Geosciences, Volume 2
  37. Considine D.M., G.D, ., 2005, Van Nostrand’s Scientific Encyclopedia, John Wiley & Sons
  38. Fritts D.C., et al., 2014, Quantifying Kelvin‐Helmholtz instability dynamics observed in noctilucent clouds: 2. Modeling and interpretation of observations, (in:) Journal of Geophysic Research Atmospheres, vol. 119, i. 5, p. 9539 – 9375


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  51. The types of noctilucent clouds
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  66. Atmospheric optics: zodiacal light
  67. Zodiacal light – All you need to know




  1. Angstrom
  2. Apsis
  3. Apsidal_precession
  4. Earth_radius
  5. Descending Moon’s Node
  6. Gamma_(eclipse)
  7. Gravity wave
  8. Greenland_ice_sheet
  9. Lunar_month
  10. Lunar_node
  11. Mesopause
  12. Mesosphere
  13. Perseids
  14. Rayleigh_(unit)
  15. Rossby_wave
  16. Saros_(astronomy)
  17. Solar_cycle
  18. Solar_cycle_25
  19. Surface_brightness
  20. Zodiacal_light

















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