Successful observation of orangutans in the wild with thermal-equipped drones

Journal of Unmanned Vehicle Systems Canadian Science Publishing 7:3 (2019) 235-257

Authors:

Claire Burke, Maisie F Rashman, Steven N Longmore, Owen McAree, Paul Glover-Kapfer, Marc Ancrenaz, Serge A Wich

The Fukang pallasite: Characterization and implications for the history of the Main‐group parent body

Meteoritics & Planetary Science Wiley 54:8 (2019) 1781-1807

Authors:

Daniella N DellaGiustina, Namrah Habib, Kenneth J Domanik, Dolores H Hill, Dante S Lauretta, Yulia S Goreva, Marvin Killgore, Yang Hexiong, Robert T Downs

Abstract:

AbstractWe report the results of a study of the Fukang pallasite that includes measurements of bulk composition, mineral chemistry, mineral structure, and petrology. Fukang is a Main‐group pallasite that consists of semiangular olivine grains (Fo 86.3) embedded in an Fe‐Ni matrix with 9–10 wt% Ni and low‐Ir (45 ppb). Olivine grains sometimes occur in large clusters up to 11 cm across. The Fe‐Ni phase is primarily kamacite with accessory taenite and plessite. Minor phases include schreibersite, chromite, merrillite, troilite, and low‐Ca pyroxene. We describe a variety of silicate inclusions enclosed in olivine that contain phases rarely or not previously reported in Main‐group pallasites, including clinopyroxene (augite), tridymite, K‐rich felsic glass, and an unknown Ca‐Cr silicate. Pressure constraints determined from tridymite (<0.4 GPa), two‐pyroxene barometry (0.39 ± 0.07 GPa), and geophysical calculations that assume pallasite formation at the core–mantle boundary (CMB), provide an upper estimate on the size of the Main‐group parent body from which Fukang originated. We conclude that Fukang originated at the CMB of a large differentiated planetesimal 400–680 km in radius.

k-means aperture optimization applied to Kepler K2 time series photometry of Titan

Publications of the Astronomical Society of the Pacific IOP Publishing 131:1002 (2019) 084505

Authors:

Ah Parker, Sm Hörst, El Ryan, Cja Howett

Abstract:

Motivated by the Kepler K2 time series of Titan, we present an aperture optimization technique for extracting photometry of saturated moving targets with high temporally and spatially varying backgrounds. Our approach uses k-means clustering to identify interleaved families of images with similar point-spread function and saturation properties, optimizes apertures for each family independently, then merges the time series through a normalization procedure. By applying k-means aperture optimization to the K2 Titan data, we achieve ≤0.33% photometric scatter in spite of background levels varying from 15% to 60% of the target's flux. We find no compelling evidence for signals attributable to atmospheric variation on the timescales sampled by these observations. We explore other potential applications of the k-means aperture optimization technique, including testing its performance on a saturated K2 eclipsing binary star. We conclude with a discussion of the potential for future continuous high-precision photometry campaigns for revealing the dynamical properties of Titan's atmosphere.

Comparing thermal infrared spectral unmixing algorithms: applications to Bennu and other airless bodies

Meteoritics and Planetary Science Wiley 54:S2 (2019)

Authors:

EC Brown, Kerri Donaldson Hanna, Neil E Bowles, VE Hamilton, BE Clark, AD Rogers, DS Lauretta, OSIRIS-REx Team

Close Cassini flybys of Saturn’s ring moons Pan, Daphnis, Atlas, Pandora, and Epimetheus

Science American Association for the Advancement of Science (AAAS) 364:6445 (2019)

Authors:

BJ Buratti, PC Thomas, E Roussos, C Howett, M Seiß, AR Hendrix, P Helfenstein, RH Brown, RN Clark, T Denk, G Filacchione, H Hoffmann, GH Jones, N Khawaja, P Kollmann, N Krupp, J Lunine, TW Momary, C Paranicas, F Postberg, M Sachse, F Spahn, J Spencer, R Srama, T Albin, KH Baines, M Ciarniello, T Economou, H-W Hsu, S Kempf, SM Krimigis, D Mitchell, G Moragas-Klostermeyer, PD Nicholson, CC Porco, H Rosenberg, J Simolka, LA Soderblom