Color, composition, and thermal environment of Kuiper Belt object (486958) Arrokoth.

Science (New York, N.Y.) 367:6481 (2020) eaay3705

Authors:

WM Grundy, MK Bird, DT Britt, JC Cook, DP Cruikshank, CJA Howett, S Krijt, IR Linscott, CB Olkin, AH Parker, S Protopapa, M Ruaud, OM Umurhan, LA Young, CM Dalle Ore, JJ Kavelaars, JT Keane, YJ Pendleton, SB Porter, F Scipioni, JR Spencer, SA Stern, AJ Verbiscer, HA Weaver, RP Binzel, MW Buie, BJ Buratti, A Cheng, AM Earle, HA Elliott, L Gabasova, GR Gladstone, ME Hill, M Horanyi, DE Jennings, AW Lunsford, DJ McComas, WB McKinnon, RL McNutt, JM Moore, JW Parker, E Quirico, DC Reuter, PM Schenk, B Schmitt, MR Showalter, KN Singer, GE Weigle, AM Zangari

Abstract:

The outer Solar System object (486958) Arrokoth (provisional designation 2014 MU69) has been largely undisturbed since its formation. We studied its surface composition using data collected by the New Horizons spacecraft. Methanol ice is present along with organic material, which may have formed through irradiation of simple molecules. Water ice was not detected. This composition indicates hydrogenation of carbon monoxide-rich ice and/or energetic processing of methane condensed on water ice grains in the cold, outer edge of the early Solar System. There are only small regional variations in color and spectra across the surface, which suggests that Arrokoth formed from a homogeneous or well-mixed reservoir of solids. Microwave thermal emission from the winter night side is consistent with a mean brightness temperature of 29 ± 5 kelvin.

The geology and geophysics of Kuiper Belt object (486958) Arrokoth.

Science (New York, N.Y.) 367:6481 (2020) eaay3999

Authors:

JR Spencer, SA Stern, JM Moore, HA Weaver, KN Singer, CB Olkin, AJ Verbiscer, WB McKinnon, J Wm Parker, RA Beyer, JT Keane, TR Lauer, SB Porter, OL White, BJ Buratti, MR El-Maarry, CM Lisse, AH Parker, HB Throop, SJ Robbins, OM Umurhan, RP Binzel, DT Britt, MW Buie, AF Cheng, DP Cruikshank, HA Elliott, GR Gladstone, WM Grundy, ME Hill, M Horanyi, DE Jennings, JJ Kavelaars, IR Linscott, DJ McComas, RL McNutt, S Protopapa, DC Reuter, PM Schenk, MR Showalter, LA Young, AM Zangari, AY Abedin, CB Beddingfield, SD Benecchi, E Bernardoni, CJ Bierson, D Borncamp, VJ Bray, AL Chaikin, RD Dhingra, C Fuentes, T Fuse, PL Gay, SDJ Gwyn, DP Hamilton, JD Hofgartner, MJ Holman, AD Howard, CJA Howett, H Karoji, DE Kaufmann, M Kinczyk, BH May, M Mountain, M Pätzold, JM Petit, MR Piquette, IN Reid, HJ Reitsema, KD Runyon, SS Sheppard, JA Stansberry, T Stryk, P Tanga, DJ Tholen, DE Trilling, LH Wasserman

Abstract:

The Cold Classical Kuiper Belt, a class of small bodies in undisturbed orbits beyond Neptune, is composed of primitive objects preserving information about Solar System formation. In January 2019, the New Horizons spacecraft flew past one of these objects, the 36-kilometer-long contact binary (486958) Arrokoth (provisional designation 2014 MU69). Images from the flyby show that Arrokoth has no detectable rings, and no satellites (larger than 180 meters in diameter) within a radius of 8000 kilometers. Arrokoth has a lightly cratered, smooth surface with complex geological features, unlike those on previously visited Solar System bodies. The density of impact craters indicates the surface dates from the formation of the Solar System. The two lobes of the contact binary have closely aligned poles and equators, constraining their accretion mechanism.

Advanced Net Flux Radiometer for the Ice Giants

Space Science Reviews Springer 216 (2020) 11

Authors:

S Aslam, RK Achterberg, SB Calcutt, V Cottini, NJ Gorius, T Hewagama, PG Irwin, CA Nixon, G Quilligan, M Roos-Serote, AA Simon, D Tran, G Villanueva

Abstract:

The design of an advanced Net Flux Radiometer (NFR), for inclusion as a payload on a future Ice Giants probe mission, is given. The Ice Giants NFR (IG-NFR) will measure the upward and downward radiation flux (hence net radiation flux), in seven spectral bands, spanning the range from solar to far infra-red wavelengths, each with a 5° Field-Of-View (FOV) and in five sequential view angles (±80°, ±45°, and 0°) as a function of altitude. IG-NFR measurements within either Uranus or Neptune’s atmospheres, using dedicated spectral filter bands will help derive radiative heating and cooling profiles, and will significantly contribute to our understanding of the planet’s atmospheric heat balance and structure, tropospheric 3-D flow, and compositions and opacities of the cloud layers. The IG-NFR uses an array of non-imaging Winston cones integrated to a matched thermopile detector Focal Plane Assembly (FPA), with individual bandpass filters, housed in a diamond windowed vacuum micro-vessel. The FPA thermopile detector signals are read out in parallel mode, amplified and processed by a multi-channel digitizer application specific integrated circuit (MCD ASIC) under field programmable gate array (FPGA) control. The vacuum micro-vessel rotates providing chopping between FOV’s of upward and downward radiation fluxes. This unique design allows for small net flux measurements in the presence of large ambient fluxes and rapidly changing ambient temperatures during the probe descent to ≥10 bar pressure.

Venus III The View After Venus Express

Springer, 2020

Authors:

Bruno Bézard, Christopher Russell, Takehiko Satoh, Suzanne Smrekar, Colin Wilson

Abstract:

The ten papers in this book, written by an international team of specialists, are the products of this effort.

Stormy water on Mars: the distribution and saturation of atmospheric water during the dusty season

Science American Association for the Advancement of Science (2020)

Authors:

AA Fedorova, F Montmessin, O Korablev, M Luginin, A Trokhimovskiy, DA Belyaev, NI Ignatiev, F Lefèvre, Juan Alday, Patrick Irwin, Kevin Olsen, J-L Bertaux, E Millour, A Määttänen, A Shakun, AV Grigoriev, A Patrakeev, S Korsa, N Kokonkov, L Baggio, F Forget, Colin Wilson

Abstract:

The loss of water from Mars to space is thought to result from the transport of water to the upper atmosphere, where it is dissociated to hydrogen and escapes the planet. Recent observations have suggested large, rapid seasonal intrusions of water into the upper atmosphere, boosting the hydrogen abundance. We use the Atmospheric Chemistry Suite on the ExoMars Trace Gas Orbiter to characterize the water distribution by altitude. Water profiles during the 2018–2019 southern spring and summer stormy seasons show that high-altitude water is preferentially supplied close to perihelion, and supersaturation occurs even when clouds are present. This implies that the potential for water to escape from Mars is higher than previously thought.