Sunho Jin, Masateru Ishiguro, Jooyeon Geem, Hiroyuki Naito, Jun Takahashi, Hiroshi Akitaya, Daisuke Kuroda, Seitaro Urakawa, Seiko Takagi, Tatsuharu Oono, Tomohiko Sekiguchi, Davide Perna, Simone Ieva, Yoonsoo P. Bach, Ryo Imazawa, Koji S. Kawabata, Makoto Watanabe, Hangbin Jo
{"title":"New evidence supporting past dust ejections from active asteroid (4015) Wilson-Harrington","authors":"Sunho Jin, Masateru Ishiguro, Jooyeon Geem, Hiroyuki Naito, Jun Takahashi, Hiroshi Akitaya, Daisuke Kuroda, Seitaro Urakawa, Seiko Takagi, Tatsuharu Oono, Tomohiko Sekiguchi, Davide Perna, Simone Ieva, Yoonsoo P. Bach, Ryo Imazawa, Koji S. Kawabata, Makoto Watanabe, Hangbin Jo","doi":"arxiv-2409.06448","DOIUrl":null,"url":null,"abstract":"Context. (4015) Wilson-Harrington (hereafter, WH) was discovered as a comet\nin 1949 but has a dynamical property consistent with that of a near-Earth\nasteroid. Although there is a report that the 1949 activity is associated with\nan ion tail, the cause of the activity has not yet been identified. Aims. This\nwork aims to reveal the mysterious comet-like activity of the near-Earth\nasteroid. Methods. We conducted new polarimetric observations of WH from May\n2022 to January 2023, reanalyses of the photographic plate images taken at the\ntime of its discovery in 1949, and dust tail simulation modelings, where the\ndust terminal velocity and ejection epoch are taken into account. Results. We\nfound that this object shows polarization characteristics similar to those of\nlow-albedo asteroids. We derived the geometric albedo ranging from pV = 0.076\n+- 0.010 to pV = 0.094 +- 0.018 from our polarimetry (the values vary depending\non the data used for fitting and the slope-albedo relationship coefficients).\nIn addition, the 1949 image showed an increase in brightness around the\nnucleus. Furthermore, we found that the color of the tail is consistent with\nsunlight, suggesting that the 1949 activity is associated with dust ejection.\nFrom the dust tail analysis, ~9 x 10^5 kg of material was ejected episodically\nat a low velocity equivalent to or even slower than the escape velocity.\nConclusions. We conclude that WH is most likely an active asteroid of main belt\norigin and that the activity in 1949 was likely triggered by mass shedding due\nto fast rotation.","PeriodicalId":501209,"journal":{"name":"arXiv - PHYS - Earth and Planetary Astrophysics","volume":"4 1","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2024-09-10","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"arXiv - PHYS - Earth and Planetary Astrophysics","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/arxiv-2409.06448","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
Abstract
Context. (4015) Wilson-Harrington (hereafter, WH) was discovered as a comet
in 1949 but has a dynamical property consistent with that of a near-Earth
asteroid. Although there is a report that the 1949 activity is associated with
an ion tail, the cause of the activity has not yet been identified. Aims. This
work aims to reveal the mysterious comet-like activity of the near-Earth
asteroid. Methods. We conducted new polarimetric observations of WH from May
2022 to January 2023, reanalyses of the photographic plate images taken at the
time of its discovery in 1949, and dust tail simulation modelings, where the
dust terminal velocity and ejection epoch are taken into account. Results. We
found that this object shows polarization characteristics similar to those of
low-albedo asteroids. We derived the geometric albedo ranging from pV = 0.076
+- 0.010 to pV = 0.094 +- 0.018 from our polarimetry (the values vary depending
on the data used for fitting and the slope-albedo relationship coefficients).
In addition, the 1949 image showed an increase in brightness around the
nucleus. Furthermore, we found that the color of the tail is consistent with
sunlight, suggesting that the 1949 activity is associated with dust ejection.
From the dust tail analysis, ~9 x 10^5 kg of material was ejected episodically
at a low velocity equivalent to or even slower than the escape velocity.
Conclusions. We conclude that WH is most likely an active asteroid of main belt
origin and that the activity in 1949 was likely triggered by mass shedding due
to fast rotation.