Leonids | |
---|---|
Pronunciation | /ˈliːənɪdz/ |
Discovery date | 902 AD (first record)[1] |
Parent body | 55P/Tempel–Tuttle[2] |
Radiant | |
Constellation | Leo |
Right ascension | 10h 17m [3] |
Declination | +21.6°[3] |
Properties | |
Occurs during | 3 November – 2 December[3] |
Date of peak | 17 November |
Velocity | 70–71[3][4] km/s |
Zenithal hourly rate | 15[3] |
The Leonids (/ˈliːənɪdz/ LEE-ə-nidz) are a prolific annual meteor shower associated with the comet Tempel–Tuttle, and are also known for their spectacular meteor storms that occur about every 33 years.[5] The Leonids get their name from the location of their radiant in the constellation Leo: the meteors appear to radiate from that point in the sky. Their proper Greek name should be Leontids with an additional ⟨t⟩ (Λεοντίδαι, Leontídai), but the word was initially constructed as a Greek/Latin hybrid[citation needed] and it has been used since.
Earth moves through meteoroid streams left from passages of a comet. The streams consist of solid particles, known as meteoroids, normally ejected by the comet as its frozen gases evaporate under the heat of the Sun when it is near the Sun – typically closer than Jupiter's orbit. Due to the retrograde orbit of 55P/Tempel–Tuttle, the Leonids are fast moving streams which encounter the path of Earth and impact at 70 km/s (43 mi/s).[3] It is the fastest annual meteor shower.[3] Larger Leonids which are about 10 mm (0.4 in) across have a mass of 0.5 g (0.02 oz) and are known for generating bright (apparent magnitude −1.5) meteors.[6] An annual Leonid shower may deposit 12 or 13 tons of particles across the entire planet.
The meteoroids left by the comet are organized in trails in orbits similar to – though different from – that of the comet. They are differentially disturbed by the planets, in particular Jupiter,[7] and to a lesser extent by radiation pressure from the Sun – the Poynting–Robertson effect and the Yarkovsky effect.[8] These trails of meteoroids cause meteor showers when Earth encounters them. Old trails are spatially not dense and compose the meteor shower with a few meteors per minute. In the case of the Leonids, that tends to peak around 18 November, but some are spread through several days on either side and the specific peak changes every year. Conversely, young trails are spatially very dense and the cause of meteor outbursts when the Earth enters one.
The Leonids also produce meteor storms (very large outbursts) about every 33 years, during which activity exceeds 1,000 meteors per hour,[9] with some events exceeding 100,000 meteors per hour,[10] in contrast to the sporadic background (5 to 8 meteors per hour) and the shower background (several meteors per hour).
Size | Apparent Magnitude | Comparable in brightness |
---|---|---|
2 mm (0.08 in) | +3.7 (visual) | Delta Ursae Majoris |
10 mm (0.4 in) | −1.5 (bright) | Sirius |
20 mm (0.8 in) | −3.8 (Fireball) | Venus |
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