Solar eclipse: the Sun, the Moon and the shadow
In the sudden darkness of the total eclipse, the solar corona unfolds its silver veils, while blazing red prominences, like glowing embers, float on the surface of the black star.
Image source: astronoo.com (new window) - AI-generated image, public domain.
Scientific summary
The Astronoo article explores the phenomenon of solar eclipses, those rare alignments in which the Moon totally or partially masks the Sun. It describes the necessary orbital conditions and the inclination of the lunar plane. The total eclipse of August 11, 1999 serves as an example to illustrate the umbral shadow, the penumbra and atmospheric cooling. Baily's beads, the red flash and the diamond ring are explained as optical signatures of the lunar topography. Finally, the gradual recession of the Moon heralds the future disappearance of total eclipses.
How does the Moon manage to mask the Sun almost perfectly?
This article is devoted to the solar eclipse, a spectacular astronomical phenomenon that occurs when the Moon comes between the Earth and the Sun. But how does the Moon manage to mask the Sun almost perfectly? The answer lies in a remarkable coincidence: the Sun is about 400 times larger than the Moon, but also about 400 times farther away, which makes their apparent diameters almost identical. This angular equality allows total, annular or partial eclipses, depending on the Earth-Moon distance. The alignment must be almost perfect, which is rare because of the 5.1° inclination of the lunar orbit. During a total eclipse, the umbral shadow projects onto Earth a narrow band where day becomes night, revealing the solar corona, prominences and Baily's beads. The eclipse of August 11, 1999, the last of the century visible in Europe, illustrates these mechanisms. In the long term, the recession of the Moon will make such total eclipses impossible.
Also worth exploring
Continue your exploration of the Universe with these topics:
Solar eclipses: perfect alignments
A historic total eclipse in Europe
On August 11, 1999, a total solar eclipse captivated Europe, Turkey and India. This rare phenomenon occurs when the Moon comes exactly between the Earth and the Sun. The shadow cast by the Moon on the Earth's surface temporarily plunged certain regions into daytime darkness.
The path of the lunar shadow
The eclipse began off the Canadian coast and crossed Western Europe as far as India. In France, it was total for about 2 minutes, with maximum occultation near Reims at 12:23 UTC. This event was the last of this intensity in the 20th century visible from continental Europe.
N.B.:
The next total eclipse to pass over Europe will occur on September 3, 2081.
The path of totality will run a little farther south and be wider than this one.
The shadow will cross France, Switzerland, Germany, Italy, Austria, Slovenia, Romania, Bulgaria, Turkey, Syria, Iraq, Iran and then the Indian Ocean, ending between the islands of Sumatra and Java.
The last 10 total solar eclipses
The table below lists the ten most recent total solar eclipses observed on Earth. The maximum duration corresponds to the longest time during which the solar disk was entirely occulted by the Moon at a given point along the path of the shadow.
| Date | Maximum duration (min) | Path of totality |
|---|---|---|
| April 8, 2024 | 4.47 | Pacific, Mexico, United States, Atlantic Canada |
| April 20, 2023 | 1.27 | Indian Ocean, Western Australia, Indonesia, Pacific |
| December 4, 2021 | 1.92 | Antarctica |
| December 14, 2020 | 2.17 | Pacific, Chile, Argentina, South Atlantic, South Africa |
| July 2, 2019 | 4.55 | South Pacific, Chile, Argentina |
| August 21, 2017 | 2.67 | Pacific, United States (coast to coast), Atlantic |
| March 9, 2016 | 4.17 | Indonesia, Pacific |
| March 20, 2015 | 2.78 | North Atlantic, Faroe Islands, Svalbard |
| November 3, 2013 | 1.67 | Atlantic, Gabon, Congo, Uganda, Kenya |
| November 13, 2012 | 4.03 | Northern Australia, South Pacific |
| July 11, 2010 | 5.20 | South Pacific, Easter Island, Chile, Argentina |
| July 22, 2009 | 6.39 | India, Nepal, China, Japan, Pacific |
| August 1, 2008 | 2.27 | Canada, Greenland, Siberia, Mongolia, China |
| March 29, 2006 | 4.07 | Brazil, Atlantic, Ghana, Togo, Benin, Nigeria, Niger, Libya, Egypt, Turkey, Georgia, Russia, Kazakhstan, Mongolia |
| April 8, 2005 | 0.42 | Pacific, Costa Rica, Panama, Colombia, Venezuela |
| November 23, 2003 | 1.57 | Antarctica |
| December 4, 2002 | 2.04 | Angola, Zambia, Zimbabwe, Mozambique, South Africa, Australia |
| June 21, 2001 | 4.57 | Angola, Zambia, Zimbabwe, Mozambique, Madagascar |
| August 11, 1999 | 2.23 | France, Europe, Turkey, India |
Black Sun: the phenomenon of total eclipses
Conditions for Sun-Earth-Moon alignment
A solar eclipse occurs only during a new moon, when the Sun, the Moon and the Earth are practically aligned on the plane of the ecliptic. Because of the Moon's orbital inclination (5.1° relative to the plane of Earth's orbit), these alignments are exceptional. The apparent diameter of the Moon can be enough to totally occult the solar disk: this is a total eclipse. The lunar shadow zone, narrow, crosses the Earth's surface at several thousand kilometers per hour.
Umbra and penumbra: the zones of the eclipse
The shadow cast by the Moon breaks down into several distinct regions. The central zone, called the umbral shadow, is a converging cone where the solar disk is entirely masked: this is where the eclipse is total. Around it extends a vast region of penumbra, where only part of the Sun is occulted, producing a partial eclipse. Between these two zones, the shadow cone may be prolonged by an antumbra, responsible for annular eclipses when the Moon is too far away to cover the entire solar disk. The width of the umbral shadow on the ground rarely exceeds 200 km, while the penumbra covers several thousand kilometers. This shadow moves at high speed, often more than 2,000 km/h, and its shape varies according to the inclination of the solar rays and the terrestrial relief. Predictive calculations of an eclipse involve celestial mechanics, the orbital parameters of the Moon and the Earth, as well as the dynamics of elliptical orbits. They make it possible to determine with precision the trajectory, duration and local times of the different phases.
When day becomes night: the spectacle of solar eclipses
Observing the solar corona
The solar eclipse of August 11, 1999 offered a precious opportunity to observe the solar corona, invisible outside these events. The rapid cooling of the ambient air, the silence of the birds, and the drop in luminosity recall the complexity of the interactions between celestial objects and their effects on our environment.
Effects on the environment and scientific measurements
From a scientific point of view, measurements of temperature, radiation, and ionospheric activity were carried out in real time. This phenomenon was also massively observed by the public and covered by the media, underlining its cultural as much as scientific impact.
Why does the Moon perfectly mask the Sun?
A cosmic coincidence: the 400 ratio
It is a remarkable coincidence of celestial mechanics: the Sun is about 400 times larger than the Moon, but it is also about 400 times farther from the Earth. Thus, their apparent diameters seen from Earth are almost equal (about 0.5 degree or 30 arc minutes).
Calculating the apparent diameter
The formula for apparent diameter is:
\(
\theta \approx \frac{D}{d}
\)
where \( D \) is the real diameter and \( d \) the distance to the observer.
- For the Sun: \( D = 1.39 \times 10^6 \) km, \( d = 1.496 \times 10^8 \) km → \( \theta_{\text{Sun}} \approx 0.0093 \) rad.
- For the Moon: \( D = 3.474 \times 10^3 \) km, \( d = 3.844 \times 10^5 \) km → \( \theta_{\text{Moon}} \approx 0.0090 \) rad.
These values explain why the Moon can perfectly mask the Sun, thus allowing total or annular eclipses depending on its distance from the Earth (perigee or apogee).
A temporary phenomenon in Earth's history
The gradual recession of the Moon
The Moon is slowly moving away from the Earth, at a rate of about 3.8 cm per year, due to tidal effects. This orbital drift means that in a few hundred million years, the Moon will appear too small to completely mask the Sun.
The future disappearance of total eclipses
Total eclipses will disappear in favor of annular eclipses. We are therefore living in an exceptional period in geological history, when orbital conditions allow total eclipses, events that are both rare, spectacular and charged with scientific meaning.
Baily's beads: the pearls of light of a total solar eclipse
Total eclipse of the Sun, where one can see Baily's beads, the red flash, the diamond ring or Airy's diamond, the Sun's chromosphere embellished by its coronal jets.
Image source: astronoo.com (new window) — AI-generated image, public domain.
What are Baily's beads?
Baily's beads are visible, not on a lunar eclipse but during a solar eclipse by the Moon. During an annular solar eclipse one can observe this phenomenon called Baily's pearls. This phenomenon is due to the topography of the Moon's surface (presence of mountains, craters, valleys, etc.). It was described strikingly by Francis Baily (1774-1844), who noted this phenomenon in 1836.
The red flash and the diamond ring
These scratches of the Moon by the Sun's light during a solar eclipse allow the pearls of sunlight to shine in some places and not in others. The irregularities of the lunar profile are perfectly known and astronomers can calculate in advance the appearance of the beads on the eclipse. Baily's beads appear briefly for a few seconds along the eclipse path. Their duration is, near the edges, 1 to 2 minutes. The Red Flash appears just after the sight of Baily's beads. This very brief passage colors the solar corona bright pink.
The red color is due to the hydrogen alpha line, which radiates at this wavelength. The diamond ring or Airy's diamond is the last portion of the Sun emerging behind the black disk of the Moon. At that moment, this image resembles a ring adorned with a diamond shining with a thousand fires. It occurs just before or just after the total eclipse.
References
- NASA Science - Eclipses (new window)
- NASA - Solar Eclipses (Goddard Space Flight Center) (new window)
- IMCCE - Institute of Celestial Mechanics and Ephemeris Computation (new window)
- Time and Date - Eclipses (maps and dates of upcoming eclipses) (new window)
- ESA - Total solar eclipse: how to follow it live from home (new window)
- Encyclopædia Britannica - Eclipse (new window)
FAQ: Everything you need to know about solar eclipses
What is a solar eclipse?
A solar eclipse is an astronomical phenomenon that occurs when the Moon comes between the Earth and the Sun, occulting all or part of the solar disk. It can only take place during a new moon, when the three bodies are aligned on the plane of the ecliptic.
Why are solar eclipses rare?
The Moon's orbit is inclined by about 5.1° relative to the plane of Earth's orbit. This angle means that the Moon is most often above or below the perfect Sun-Earth-Moon alignment. Solar eclipses therefore occur only a few times a year, and the path of totality touches only a tiny part of the Earth's surface.
What is the difference between a total, annular and partial eclipse?
A total eclipse occurs when the Moon entirely masks the solar disk, revealing the corona. An annular eclipse occurs when the Moon, farther from the Earth, appears too small to cover the whole Sun, leaving a ring of light visible. A partial eclipse shows only a partial occultation of the solar disk.
Why should you never look at a solar eclipse with the naked eye?
Solar radiation, even partially occulted, remains extremely intense. Observing it without suitable protection (certified special glasses) can cause irreversible retinal damage, often without immediate pain. Ordinary sunglasses are not enough.
How long does a total solar eclipse last?
The totality phase generally lasts between a few seconds and about 7 minutes at most, depending on the geometry of the alignment. The total duration of the event (partial phases included) can extend over several hours.
Why can the Moon mask the Sun although it is much smaller?
The Sun is about 400 times larger than the Moon, but it is also about 400 times farther from the Earth. This proportion makes their apparent diameters, seen from Earth, almost identical (about 0.5°). It is this cosmic coincidence that makes total eclipses possible.
Race to the Shadow: The Total Eclipse 2026
Red Moon and Blood Moon: The Earth's Atmosphere to Blame
Solar Eclipse: The Sun, the Moon, and the Shadow
Baily's Beads: Fleeting Jewels of the Solar Eclipse
Eclipses explained by the plane of the orbit
The eclipse seen from above: what satellites reveal about the Sun
Transit of Venus on June 6, 2012
Lunar Transit Phenomenon: A Small-Scale Eclipse?
Impact theory at the origin of the Moon
Periodicity and Repetition of Eclipses
The annular eclipse of January 15, 2010: the longest ring of fire of the century