Eclipse time variations in the post-common envelope binary V470 Cam

Monthly Notices of the Royal Astronomical Society Oxford University Press (OUP) 499:3 (2020) 3071-3084

Authors:

O Sale, D Bogensberger, F Clarke, AE Lynas-Gray

Author Correction: Shape of (101955) Bennu indicative of a rubble pile with internal stiffness

Nature Geoscience Springer Nature 13:11 (2020) 764-764

Authors:

OS Barnouin, MG Daly, EE Palmer, RW Gaskell, JR Weirich, CL Johnson, MM Al Asad, JH Roberts, ME Perry, HCM Susorney, RT Daly, EB Bierhaus, JA Seabrook, RC Espiritu, AH Nair, L Nguyen, GA Neumann, CM Ernst, WV Boynton, MC Nolan, CD Adam, MC Moreau, B Rizk, CY Drouet D’Aubigny, ER Jawin, KJ Walsh, P Michel, SR Schwartz, R-L Ballouz, EM Mazarico, DJ Scheeres, JW McMahon, WF Bottke, S Sugita, N Hirata, N Hirata, S-I Watanabe, KN Burke, DN DellaGiustina, CA Bennett, DS Lauretta

Introduction to Icarus special issue “From Mars Express to ExoMars”

Icarus Elsevier 353 (2020) 114118

Authors:

Miguel A Lopez-Valverde, Dmitrij V Titov, Colin F Wilson

Global quieting of high-frequency seismic noise due to COVID-19 pandemic lockdown measures

Science American Association for the Advancement of Science (AAAS) 369:6509 (2020) 1338-1343

Authors:

Thomas Lecocq, Stephen P Hicks, Koen Van Noten, Kasper van Wijk, Paula Koelemeijer, Raphael SM De Plaen, Frédérick Massin, Gregor Hillers, Robert E Anthony, Maria-Theresia Apoloner, Mario Arroyo-Solórzano, Jelle D Assink, Pinar Büyükakpınar, Andrea Cannata, Flavio Cannavo, Sebastian Carrasco, Corentin Caudron, Esteban J Chaves, David G Cornwell, David Craig, Olivier FC den Ouden, Jordi Diaz, Stefanie Donner, Christos P Evangelidis, Läslo Evers, Benoit Fauville, Gonzalo A Fernandez, Dimitrios Giannopoulos, Steven J Gibbons, Társilo Girona, Bogdan Grecu, Marc Grunberg, György Hetényi, Anna Horleston, Adolfo Inza, Jessica CE Irving, Mohammadreza Jamalreyhani, Alan Kafka, Mathijs R Koymans, Celeste R Labedz, Eric Larose, Nathaniel J Lindsey, Mika McKinnon, Tobias Megies, Meghan S Miller, William Minarik, Louis Moresi, Víctor H Márquez-Ramírez, Martin Möllhoff, Ian M Nesbitt, Shankho Niyogi, Javier Ojeda, Adrien Oth, Simon Proud, Jay Pulli, Lise Retailleau, Annukka E Rintamäki, Claudio Satriano, Martha K Savage, Shahar Shani-Kadmiel, Reinoud Sleeman, Efthimios Sokos, Klaus Stammler, Alexander E Stott, Shiba Subedi, Mathilde B Sørensen, Taka'aki Taira, Mar Tapia, Fatih Turhan, Ben van der Pluijm, Mark Vanstone, Jerome Vergne, Tommi AT Vuorinen, Tristram Warren, Joachim Wassermann, Han Xiao

Studying the composition and mineralogy of the hermean surface with the Mercury Radiometer and Thermal Infrared Spectrometer (MERTIS) for the BepiColombo mission: an update

Space Science Reviews Springer 216:6 (2020) 110

Authors:

H Hiesinger, J Helbert, G Alemanno, Ke Bauch, M D’Amore, A Maturilli, A Morlok, Mp Reitze, C Stangarone, An Stojic, I Varatharajan, I Weber, G Arnold, M Banaszkiewicz, K Bauch, J Benkhoff, A Bischoff, M Blecka, N Bowles, S Calcutt, L Colangeli, S Erard, S Fonti, Bt Greenhagen, O Groussain, H Hirsch, J Jahn, R Killen, J Knollenberg, E Kührt, E Lorenz, I Mann, U Mall, A Maturilli, A Morlok, L Moroz, G Peter, M Rataj, M Robinson, W Skrbek, T Spohn, A Sprague, D Stöffler, A Stojic, F Taylor, I Varatharajan, H Venus, J Warrell, I Walter, I Weber

Abstract:

Launched onboard the BepiColombo Mercury Planetary Orbiter (MPO) in October 2018, the Mercury Radiometer and Thermal Infrared Spectrometer (MERTIS) is on its way to planet Mercury. MERTIS consists of a push-broom IR-spectrometer (TIS) and a radiometer (TIR), which operate in the wavelength regions of 7-14 μm and 7-40 μm, respectively. This wavelength region is characterized by several diagnostic spectral signatures: the Christiansen feature (CF), Reststrahlen bands (RB), and the Transparency feature (TF), which will allow us to identify and map rock-forming silicates, sulfides as well as other minerals. Thus, the instrument is particularly well-suited to study the mineralogy and composition of the hermean surface at a spatial resolution of about 500 m globally and better than 500 m for approximately 5-10% of the surface. The instrument is fully functional onboard the BepiColombo spacecraft and exceeds all requirements (e.g., mass, power, performance). To prepare for the science phase at Mercury, the team developed an innovative operations plan to maximize the scientific output while at the same time saving spacecraft resources (e.g., data downlink). The upcoming fly-bys will be excellent opportunities to further test and adapt our software and operational procedures. In summary, the team is undertaking action at multiple levels, including performing a comprehensive suite of spectroscopic measurements in our laboratories on relevant analog materials, performing extensive spectral modeling, examining space weathering effects, and modeling the thermal behavior of the hermean surface.