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C/1907 G1 (Grigg–Mellish)

Long-period comet From Wikipedia, the free encyclopedia

C/1907 G1 (Grigg–Mellish)
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C/1907 G1 (Grigg–Mellish) is a long-period comet discovered independently by John Grigg and John E. Mellish in April 1907. The comet has been identified as the parent body of the delta Pavonids meteor shower.

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Discovery and observations

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John Grigg, in New Zealand, discovered a nebulous object near the star α Cae on 8 April 1907, however the discovery wasn't communicated quickly enough for observers in the southern hemisphere to confirm the discovery.[4] The comet was found independently by amateur astronomer John E. Mellish, from Madison, Wisconsin, on 14 April. The comet had an apparent magnitude of 11 upon discovery.[5] The comet was also spotted by Edward Emerson Barnard in a photographic plate exposed on 13 April while he was searching for comet C/1907 E1 (Giacobini). The comet formed a trail 13.6 arcminutes long during the one hour the plate was exposed.[6] The comet was reported to have a coma two arcminutes across and a broad tail 8 arcminutes long on 16 April. The comet faded rapidly and it was difficult to measure with the 36-inch telescope of Lick Observatory on 7 May.[7]

The comet was found to have a similar orbit to comet C/1742 C1,[8] however comet Grigg–Mellish is intrinsically fainter than that comet. The comet's orbit passes very close to Earth, at a distance of 0.003 AU (0.45 million km; 0.28 million mi); Earth passes that point on 30 March. Due to the small minimum orbit intersection distance, it was suggested to be a source of meteors with a radiant point at R.A. = 20.63h , DEC = –60.4° and a speed of Vg = 59.0 km/s.[9]

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Meteor shower

Comet Grigg–Mellish has been identified as the parent body of the delta Pavonids meteor shower. The shower has a zenithal hourly rate (ZHR) of 5 meteors per hour and peaks at March 31. An outburst was observed in 2019. The orbit of the meteors indicates that comet has an orbital period of 447 ± 80 years.[9]

References

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