Cassini composite infrared spectrometer: correcting an offset error and refining the pointing parameters for the midinfrared detectors.

Applied optics 62:22 (2023) 5882-5888

Authors:

John C Pearl, Conor A Nixon, Donald E Jennings, Shahid Aslam, Simon Calcutt, Monte S Kaelberer, Nicolas Gorius, Richard K Achterberg, Paul N Romani, Gordon L Bjoraker, Michael Flasar

Abstract:

Based on preflight laboratory testing, an unexpectedly large positional offset between the two midinfrared (mid-IR) detector arrays in the Cassini composite infrared spectrometer (CIRS) instrument has been noted in the literature. A much smaller offset was measured in-flight. We investigate this discrepancy by estimating several spatial relationships among the detectors and comparing these results with three independent data sets. This enables us to infer the probable cause of this offset and to derive a new reduced value. We comment on the effect that this change could have on previously published results involving CIRS data. We also present a graphical display of the arrays projected on the sky as CIRS would see it.

Cassini composite infrared spectrometer: correcting an offset error and refining the pointing parameters for the midinfrared detectors: publisher's note.

Applied optics 62:23 (2023) 6298

Authors:

John C Pearl, Conor A Nixon, Donald E Jennings, Shahid Aslam, Simon Calcutt, Monte S Kaelberer, Nicolas Gorius, Richard K Achterberg, Paul N Romani, Gordon L Bjoraker, Michael Flasar

Abstract:

This publisher's note serves to correct Appl. Opt.62, 5882 (2023).APOPAI0003-693510.1364/AO.491970.

Nonthermal Hydrogen Loss at Mars: Contributions of Photochemical Mechanisms to Escape and Identification of Key Processes

Journal of Geophysical Research Planets American Geophysical Union (AGU) 128:8 (2023)

Authors:

Bethan S Gregory, Michael S Chaffin, Rodney D Elliott, Justin Deighan, Hannes Gröller, Eryn Cangi

Solar Energetic Particle Events Detected in the Housekeeping Data of the European Space Agency's Spacecraft Flotilla in the Solar System

Space Weather American Geophysical Union (AGU) 21:8 (2023)

Authors:

Beatriz Sánchez‐Cano, Olivier Witasse, Elise W Knutsen, Dikshita Meggi, Shayla Viet, Mark Lester, Robert F Wimmer‐Schweingruber, Marco Pinto, Richard Moissl, Johannes Benkhoff, Hermann Opgenoorth, Uli Auster, Jos de Brujine, Peter Collins, Guido De Marchi, David Fischer, Yoshifumi Futaana, James Godfrey, Daniel Heyner, Mats Holmstrom, Andrew Johnstone, Simon Joyce, Daniel Lakey, Santa Martinez, David Milligan, Elsa Montagnon, Daniel Müller, Stefano A Livi, Timo Prusti, Jim Raines, Ingo Richter, Daniel Schmid, Peter Schmitz, Håkan Svedhem, Matt GGT Taylor, Elena Tremolizzo, Dimitri Titov, Colin Wilson, Simon Wood, Joe Zender

Bidirectional reflectance distribution function measurements of the Winchcombe meteorite using the Visible Oxford Space Environment Goniometer

Meteoritics and Planetary Science Wiley 59:5 (2023) 1029-1042

Authors:

Rowan Curtis, Hc Bates, TJ Warren, KA Shirley, EC Brown, Aj King, NE Bowles

Abstract:

A laboratory study was performed using the Visible Oxford Space Environment Goniometer in which the broadband (350–1250 nm) bidirectional reflectance distribution function (BRDF) of the Winchcombe meteorite was measured, across a range of viewing angles—reflectance: 0°–70°, in steps of 5°; incidence: 15°, 30°, 45°, and 60°; and azimuthal: 0°, 90°, and 180°. The BRDF dataset was fitted using the Hapke BRDF model to (1) provide a method of comparison to other meteorites and asteroids, and (2) to produce Hapke parameter values that can be used to extrapolate the BRDF to all angles. The study deduced the following Hapke parameters for Winchcombe: w = 0.152 ± 0.030, b = 0.633 ± 0.064, and hS = 0.016 ± 0.008, demonstrating that it has a similar w value to Tagish Lake (0.157 ± 0.020) and a similar b value to Orgueil (0.671 ± 0.090). Importantly, the surface profile of the sample was characterized using an Alicona 3D® instrument, allowing two of the free parameters within the Hapke model φ and (Formula presented.), which represent porosity and surface roughness, respectively, to be constrained as φ = 0.649 ± 0.023 and (Formula presented.) = 16.113° (at 500 μm size scale). This work serves as part of the characterization process for Winchcombe and provides a reference photometry dataset for current and future asteroid missions.