Comet C/2011 W3 (Lovejoy): Orbit Determination, Outbursts, Disintegration of Nucleus, Dust-Tail Morphology, and Relationship to New Cluster of Bright Sungrazers
Zdenek Sekanina, Paul W. Chodas

TL;DR
This paper details the physical and orbital analysis of comet C/2011 W3 Lovejoy, revealing its disintegration process, dust tail morphology, and its connection to a new cluster of sungrazers, challenging existing models of comet structure.
Contribution
It introduces a novel method for orbit determination based on tail intersection points and links C/2011 W3 to a new Kreutz sungrazer cluster, providing insights into comet disintegration.
Findings
The comet's orbital period is approximately 698 years.
Disintegration was caused by thermal stress after perihelion.
Dust tail analysis indicates submicron silicate grains.
Abstract
We describe the physical and orbital properties of C/2011 W3. After surviving perihelion, the comet underwent major changes (permanent loss of nuclear condensation, formation of spine tail). The process of disintegration culminated with an outburst on December 17.6 (T+1.6 d) and this delayed response is inconsistent with the rubble pile model. Probable cause was thermal stress from the heat pulse into the nucleus after perihelion, which could also produce fragmentation of sungrazers far from the Sun. The spine tail was a synchronic feature, made up of dust released at <30 m/s. Since the nucleus would have been located on the synchrone, we computed the astrometric positions of the missing nucleus as the coordinates of the points of intersection of the spine tail's axis with lines of forced orbital-period variation, derived from orbital solutions based on preperihelion astrometry from the…
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