Skip to content
Home

Comet

Comets are small icy bodies that orbit the Sun, developing glowing comas and tails when heated. They originate in distant reservoirs and reveal information about the early solar system.

A comet is a small celestial body composed primarily of volatile ices mixed with dust and rock. Early descriptions called them "dirty snowballs" because they contain frozen gases and particulate material in a compact nucleus. Modern observations show a range of sizes, shapes and surface compositions. A concise description of their makeup is that comets are balls of ice and dust: composition overview containing water ice, frozen carbon compounds and silicate grains (ice and volatiles) embedded in a dark matrix, traveling through outer space.

Image gallery

10 Images

Structure and visible features

The dense, solid core of a comet is called the nucleus. When a comet approaches the Sun, solar heating causes ices to sublimate and release gas and dust, forming a fuzzy atmosphere called the coma and often one or more tails. Tails are not fixed behind the nucleus: an ion (gas) tail points away from the Sun because it is shaped by the solar wind, while a dust tail is pushed by sunlight and follows a curved path. A comet's nucleus typically has a very low reflectivity; for example, observations of Halley's Comet showed a surface that reflected only a few percent of incident light. These differences distinguish comets from rocky asteroids (asteroids), which lack volatile-driven comae and bright tails.

Origins and orbits

Comets originate in two principal reservoirs at the fringes of the solar system. Short-period comets, with orbits measured in decades to centuries, are commonly associated with the Kuiper belt and scattered disc beyond Neptune (Kuiper belt). Long-period comets, which may take thousands or millions of years to return, are thought to arise from the distant, roughly spherical Oort cloud. Many comets have orbital inclinations that carry them far from the plane of the planets; their orbital inclinations are often high and not confined to the ecliptic plane (orbital inclinations).

Behavior, lifetimes and fragmentation

As comets repeatedly pass near the Sun they lose material and can become inactive or disintegrate. Some break apart under thermal stress, tidal forces or internal gas pressure. Historical examples include Comet Biela, which fragmented in the 19th century, and Comet Shoemaker–Levy 9, whose pieces impacted Jupiter in 1994 (Shoemaker–Levy 9). Groups of comets observed to follow similar orbits are often interpreted by astronomers as fragments from a single parent body (astronomers' studies).

Observation, study and examples

Comets have been important both culturally and scientifically. They were once regarded as omens but are now valuable probes of primordial material from the early solar system. Telescopic studies and spacecraft encounters have transformed our understanding: close flybys and missions such as Giotto and Rosetta provided in‑situ data and images of nuclei. Scientific summaries and mission pages describe these efforts (mission archives). The dark, low-reflectance surfaces of many nuclei relate to their albedo and the distribution of organic-rich material.

Why comets matter

Comets supply unique information about the composition and physical conditions of the early solar nebula because they have preserved volatile compounds that are otherwise rare in planetary materials. Studying cometary chemistry and dynamics informs models of planetary formation and delivery of water and organics to the inner solar system. Observational techniques range from ground-based telescopes to space missions, and amateur observers still play a role when bright comets visit the inner solar system.

History of comet research

Main article: Comet research

Even in early times, comets aroused great interest because they appear suddenly and behave completely differently from other celestial bodies. In ancient times and up to the Middle Ages, they were therefore often regarded as messengers of fate or signs of the gods.

In antiquity, during the observation of a conjunction with the naked eye, there apparently occurred a fusion of a planet with a star, which is mentioned by Aristotle in his writing "Meteorologica" and was regarded as a possible cause for the formation of comets. It is apparently the event that took place in Greece about ten years before the writing, in the morning hours of July 13, 360 B.C., on the eastern horizon, where the smallest angular distance between the ecliptic star Wasat and the planet Jupiter in the constellation Gemini was only about 20 minutes of arc. Based on the fact that no comet was formed in this event, Aristotle ruled out such events as a cause for the appearance of comets. Aristotle and Ptolemy therefore considered comets to be evaporations of the Earth's atmosphere.

Only Regiomontanus recognized independent celestial bodies in the comets and tried to measure an orbit in 1472. The oldest printed text on comets is probably the Tractatus de Cometis, published in Beromünster in 1472 and in Venice in 1474, by the Zurich city doctor Eberhard Schleusinger, who was born in Goßmannsdorf near Hofheim in Lower Franconia and whose work forms the basis for Johannes Lichtenberger's Pronosticatio. Tycho Brahe's discovery that comets are not phenomena of the Earth's atmosphere can be regarded as the beginning of scientific comet research. For he determined with the comet of 1577 that it must be at least 230 earth radii away. However, it took many decades before this assumption was accepted, and even Galileo contradicted it. In 1682, Edmond Halley succeeded in proving the tail star that appeared in that year to be a periodically recurring celestial body. The comet, which was also observed in 1607, 1531 and 1456, moves on an elongated ellipse around the sun in 76 years. Nowadays an average of 20-30 comets are discovered per year.

The state of knowledge about comets around the middle of the 19th century can be taken from Scheffel's humorous song Der Komet: "Even Humboldt, the old man of explorative power, ...: 'It fills the comet, much thinner than foam, With all-smallest mass the very largest space?'"

Overview

Characterization

Comets are divided into aperiodic comets and periodic comets on the basis of their appearance interval. The latter are divided according to their orbital periods into long-period and short-period comets.

Aperiodic comets

Comets, which - due to their parabolic or hyperbolic orbit - certainly do not recur, or single observations, about which - due to lack of exact orbit determination - no statement can be made yet.

Periodic comets

Comets whose recurrence is assured by their orbital elements, i.e. which orbit the Sun in a stable orbit - at least for a certain period of time.

  • Long-period comets with an orbital period of more than 200 years probably come from Oort's Cloud, their orbital inclinations are statistically distributed and they orbit the Sun both in the same sense of orbit as the planets (prograde) and in the opposite direction to the planetary orbits (retrograde). The eccentricities of their orbits are close to 1 - but the comets are usually still bound to the Sun by gravity, although it takes them up to 100 million years to complete their orbits. Eccentricities greater than 1 (hyperbolic orbits) are rare and are caused mainly by orbital perturbations as they pass the major planets. These comets then theoretically do not return close to the Sun, but leave the solar system. In the outer part of the planetary system, however, even small forces are sufficient to make the orbit elliptical again.
  • Short-period comets with orbital periods of less than 200 years probably originate from the Kuiper belt. They usually move in the usual sense of orbit and their inclination is on average about 20°, so they are close to the ecliptic. For more than half of the short-period comets the largest solar distance (aphelion) near the orbit of Jupiter is 5 and 6 astronomical units (Jupiter family). These are originally longer-period comets whose orbits have been altered by the influence of Jupiter's gravity.

Designation

Main article: Naming of asteroids and comets

Newly discovered comets are first given a name by the International Astronomical Union, consisting of the year of discovery and a capital letter, starting with A on 1 January and B on 16 January in a half-monthly rhythm (until Y on 16 December, the letter I is skipped) after the date of discovery. In addition, a number is added so that several comets can be distinguished in the half month. As soon as the orbital elements of the comet are determined more exactly, another letter is prefixed to the name according to the following system:

P

the orbital period is less than 200 years or at least two confirmed observations of the perihelion passage (periodic comet)

C

The orbital period is greater than 200 years.

X

The trajectory cannot be determined.

D

Periodic comet that was lost or no longer exists.

A

It is subsequently discovered that it is not a comet, but an asteroid.

Comet Hyakutake, for example, is also listed under the designation C/1996 B2. So Hyakutake was the second comet discovered in the second half of January 1996. Its orbital period is greater than 200 years.

Usually a comet is additionally named after its discoverers, for example D/1993 F2 is also called Shoemaker-Levy 9 - it is the ninth comet discovered by Eugene and Carolyn Shoemaker together with David H. Levy.

Comet Orbits

Since only short orbital arcs have been observed for newly discovered comets, parabolic orbits are calculated first. However, since a parabola is only a mathematical limiting case and cannot occur as such in nature (any disturbance, no matter how tiny, turns it into an ellipse or a hyperbola), comets whose orbital eccentricity is given as e = 1.0 (= parabola). actually run either on ellipses (e < 1.0) or on hyperbolas (e > 1.0). With longer observation and the acquisition of additional astrometric positions, it can then be decided whether they are ellipses or hyperbolas.

From about 660 examined comets the following distribution can be seen: 43 % parabolas, 25 % long period ellipses (orbital period over 200 years), 17 % short period ellipses (orbital period up to 200 years) and 15 % hyperbolas. However, the high proportion of parabolas is due to the too short observation period of many cometary phenomena, where long-period ellipses cannot be distinguished from a parabola. With a longer visibility of 240 to 500 days only 3% of the comets probably still describe a parabolic orbit. Thus the ellipses are likely to be predominant.

Discovery and observation of comets

Main article: Visibility of comets

While until 1900 about 5 to 10 new comets were discovered per year, this number has risen to more than 20 in the meantime. This is mainly due to automatic sky surveys and observations by space probes. But there are also amateur astronomers who have specialized in comet search, especially in Japan and Australia.

The most successful was the New Zealander William Bradfield with 17 discoveries between 1972 and 1995, all of which were named after him. He systematically searched the twilight sky up to 90° solar separation and spent about 100 hours a year on it.

For visual observations, fast binoculars or a special comet finder are suitable. A low magnification at high luminosity is important to preserve the relatively low surface brightness of the comet (similar to nebula observations). The exit pupil should therefore correspond to that of the dark-adapted eye (about 7 mm).

Today, cameras with highly sensitive CCD sensors are mostly used for photography. For detailed photographs (e.g. of the structure of the comet's tail), the camera does not track the stars, but the comet itself by means of an approximate orbit calculation. Most of them are still in the outer solar system when they are discovered and appear only as a diffuse star of 15th to 20th magnitude.

Space probes to comets

The following table lists some comets that have been visited or are planned to be visited by space probes:

Name

Discovery

Space probe

Date

Closest approach
(km)

Comments

Borrelly

1904

Deep Space 1

2001

2200

Flyby

Giacobini-Zinner

1900

ICE

1985

7800

Flyby

Grigg-Skjellerup

1902

Giotto

1992

200

Flyby

Halley

known since ancient times

Giotto

1986

596

Flyby

Hartley 2

1986

Deep Impact,
Extended Mission EPOXI

2010

700

flyby,
smallest comet studied

Temple 1

1867

deep impact

2005

500;
impactor penetrates

Impact + flyby

Churyumov-Gerasimenko

1969

Rosetta

2014

6 or 0

Orbit of Rosetta; landing of lander Philae on Nov. 12, 2014,
Rosetta's descent to the core on Sept. 30, 2016.

Game 2

1978

Stardust

2004

240

Fly-by and return to Earth (Sample return mission)

For comparison, June 2018 Hayabusa 2 probe approaches within a few kilometers of asteroid Ryugu.

Questions and answers

Q: What is a comet?

A: A comet is a ball of mostly ice that moves around in outer space. They are often described as "dirty snowballs".

Q: How do comets differ from asteroids?

A: Comets have higher orbital inclinations than asteroids, and they are usually found farther away from the ecliptic plane where most solar system objects are located.

Q: What causes comets to have tails?

A: Comets have long tails because the Sun melts the ice, creating gas and dust which is then blown away by the solar wind.

Q: What is the nucleus of a comet?

A: The nucleus of a comet is its hard centre, and it has one of the lowest albedos (reflectivity) in the solar system. When light shone on Halley's Comet's nucleus, only 4% was reflected back to us.

Q: Are there different types of comets?

A: Yes, there are periodic comets which visit again and again, and non-periodic or single-apparition comets which visit only once. Some comets also orbit together in groups which astronomers think may be broken pieces that used to be one object.

Q: Can comets break up?

A: Yes, some comets can break up over time due to gravitational forces or collisions with other objects such as planets or asteroids. For example, Comet Biela broke up in the 19th century and Comet Shoemaker-Levy 9 broke up before hitting Jupiter in 1994.

Q: Where do most comets come from?

A: Most comets come from the Kuiper belt which is very far away from the Sun but close enough for us to see them at night when they pass near Earth.

Related articles

Author

AlegsaOnline.com Comet

URL: https://en.alegsaonline.com/art/21917

Share