| Autor: |
C. M. Lisse, J. K. Steckloff, D. Prialnik, M. Womack, O. Harrington Pinto, G. Sarid, Y. R. Fernandez, C. A. Schambeau, T. Kareta, N. H. Samarasinha, W. Harris, K. Volk, L. M. Woodney, D. P. Cruikshank, S. A. Sandford |
| Rok vydání: |
2022 |
| Předmět: |
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| Zdroj: |
The Planetary Science Journal. 3:251 |
| ISSN: |
2632-3338 |
| DOI: |
10.3847/psj/ac9468 |
| Popis: |
Centaur 29P/Schwassmann–Wachmann 1 (SW1) is a highly active object orbiting in the transitional “Gateway” region between the Centaur and Jupiter-family comet (JFC) regions. SW1 is unique among the Centaurs in that it experiences quasi-regular major outbursts and produces CO emission continuously; however, the source of the CO is unclear. We argue that, due to its very large size (∼32 km radius), SW1 is likely still responding, via amorphous water ice (AWI) conversion to crystalline water ice (CWI), to the “sudden” change in its external thermal environment produced by its Myrs-long dynamical migration from the Kuiper Belt to its current location at the inner edge of the Centaur region. It is this conversion process that is the source of the abundant CO and dust released from the object during its quiescent and outburst phases. If correct, these arguments have a number of important predictions testable via remote sensing and in situ spacecraft characterization, including the quick release on Myr timescales of CO from AWI conversion for any few kilometer-scale scattered disk Kuiper Belt Objects transiting into the inner system; that to date SW1 has only converted between 50% and 65% of its nuclear AWI to CWI; that volume changes on AWI conversion could have caused subsidence and cave-ins, but not significant mass wasting or crater loss; that SW1's coma should contain abundant amounts of CWI+CO2 “dust” particles; and that when SW1 transits into the inner system within the next 10,000 yr, it will be a very different kind of JFC. |
| Databáze: |
OpenAIRE |
| Externí odkaz: |
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