Issue |
A&A
Volume 541, May 2012
|
|
---|---|---|
Article Number | A70 | |
Number of page(s) | 10 | |
Section | Planets and planetary systems | |
DOI | https://doi.org/10.1051/0004-6361/201117950 | |
Published online | 01 May 2012 |
Simultaneous Swift X-ray and UV views of comet C/2007 N3 (Lulin)
1 Department of Physics and Astronomy, University of Leicester, Leicester, LE1 1RH, UK
e-mail: jac48@star.le.ac.uk; amr30@star.le.ac.uk
2 Department of Astronomy, University of Maryland, College Park, MD 20742-2421, USA
e-mail: dennis@astro.umd.edu
3 Astrophysics Science Division, Code 662, NASA Goddard Space Flight Center, Greenbelt, MD 20771, USA
e-mail: stefan.m.immler@nasa.gov
Received: 25 August 2011
Accepted: 6 March 2012
Aims. We present an analysis of simultaneous X-Ray and UV observations of comet C/2007 N3 (Lulin) taken on three days between January 2009 and March 2009 using the Swift observatory.
Methods. For our X-ray observations, we used basic transforms to account for the movement of the comet to allow the combination of all available data to produce an exposure-corrected image. We fit a simple model to the extracted spectrum and measured an X-ray flux of 4.3 ± 1.3 × 10-13 erg cm-2 s-1 in the 0.3 to 1 keV band. In the UV, we acquired large-aperture photometry and used a coma model to derive water production rates given assumptions regarding the distribution of water and its dissociation into OH molecules about the comet’s nucleus.
Results. We compare and discuss the X-ray and UV morphology of the comet. We show that the peak of the cometary X-ray emission is offset sunward of the UV peak emission, assumed to be the nucleus, by approximately 35 000 km. The offset observed, the shape of X-ray emission and the decrease of the X-ray emission comet-side of the peak, suggested that the comet was indeed collisionally thick to charge exchange, as expected from our measurements of the comet’s water production rate (6–8 × 1028 mol s-1). The X-ray spectrum is consistent with solar wind charge exchange emission, and the comet most likely interacted with a solar wind depleted of very highly ionised oxygen. We show that the measured X-ray lightcurve can be very well explained by variations in the comet’s gas production rates, the observing geometry and variations in the solar wind flux.
Key words: X-rays: general / comets: individual: C/2007 N3 (Lulin) / ultraviolet: general
© ESO, 2012
Current usage metrics show cumulative count of Article Views (full-text article views including HTML views, PDF and ePub downloads, according to the available data) and Abstracts Views on Vision4Press platform.
Data correspond to usage on the plateform after 2015. The current usage metrics is available 48-96 hours after online publication and is updated daily on week days.
Initial download of the metrics may take a while.