Watching a Comet Turn On: High Spectral Resolving Power Observations of Comet C/2017 K2 (PanSTARRS)
Anita L. Cochran, Adam J. McKay, Youssef Moulane
TL;DR
Using high-resolution optical spectroscopy from McDonald Observatory and Keck, the study tracks the onset of gas-phase emission in comet C/2017 K2 (PanSTARRS) as it approaches perihelion. CN emission appears first at Rh=3.39 au, followed by detections of C3, CH, C2, and NH2 at progressively smaller distances, while forbidden oxygen lines indicate H$_2$O as a primary parent with modest distance-dependent variation. JWST observations near 2.35 au reveal CO and CO$_2$ contributions alongside dominant H$_2$O, and ground-based data suggest elevated volatile-to-water ratios, pointing to a more complex, possibly heterogeneous volatile inventory. The outbound detections of CN beyond 4 au imply clumpy, volatile-driven activity on an Oort Cloud comet, challenging the notion that water is the sole driver of early activity and highlighting the value of far-distance, high-resolution spectroscopy for understanding cometary volatiles.
Abstract
We report high spectral resolving power optical observations of comet C/2017\,K2 (PanSTARRS) as it approached the Sun. This comet was discovered when it was 16\,{\sc au} from the Sun. At discovery, the comet had a large and relatively bright coma. However, the spectrum at discovery showed only signatures of dust. We used the coud{é} spectrograph on the McDonald Observatory 2.7\,m telescope to obtain spectra, starting when the comet was at a heliocentric distance of 5.06\,{\sc au} and following it until 2.47\,{\sc au}, to determine what spectral features would appear at each heliocentric distance. The first heliocentric distance for which we detected any emission from the gas was 3.39\,{\sc au}, when we first detected CN. As the comet continued inward towards the Sun, various other species were detected. We discuss the implications of the early turn-on of CN and of species first appearing at different heliocentric distances in the context of control of the activity by water.
