On the detectability of trace chemical species in the martian atmosphere using gas correlation filter radiometry
Icarus Elsevier 260 (2015) 103-127
The Pluto system: Initial results from its exploration by New Horizons
(2015)
The Subaru–XMM-Newton Deep Survey (SXDS). VIII. Multi-wavelength identification, optical/NIR spectroscopic properties, and photometric redshifts of X-ray sources†
Publications of the Astronomical Society of Japan Oxford University Press (OUP) 67:5 (2015) 82
The Pluto system: Initial results from its exploration by New Horizons.
Science (New York, N.Y.) 350:6258 (2015) aad1815
Abstract:
The Pluto system was recently explored by NASA's New Horizons spacecraft, making closest approach on 14 July 2015. Pluto's surface displays diverse landforms, terrain ages, albedos, colors, and composition gradients. Evidence is found for a water-ice crust, geologically young surface units, surface ice convection, wind streaks, volatile transport, and glacial flow. Pluto's atmosphere is highly extended, with trace hydrocarbons, a global haze layer, and a surface pressure near 10 microbars. Pluto's diverse surface geology and long-term activity raise fundamental questions about how small planets remain active many billions of years after formation. Pluto's large moon Charon displays tectonics and evidence for a heterogeneous crustal composition; its north pole displays puzzling dark terrain. Small satellites Hydra and Nix have higher albedos than expected.HSIM: a simulation pipeline for the HARMONI integral field spectrograph on the European ELT
Monthly Notices of the Royal Astronomical Society Oxford University Press 453:4 (2015) 3754-3765