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Mars's Red (575–625 nm) Seasonal Approximate Reflectivity Averaged Over Mars Years 24–28 From Mars Orbiter Camera
Author(s) -
Robbins Stuart J.
Publication year - 2020
Publication title -
journal of geophysical research: planets
Language(s) - English
Resource type - Journals
eISSN - 2169-9100
pISSN - 2169-9097
DOI - 10.1029/2019je006231
Subject(s) - mars exploration program , orbiter , tharsis , remote sensing , albedo (alchemy) , mars landing , mars rover , martian , exploration of mars , astrobiology , geology , physics , astronomy , art , performance art , art history
The Mars Global Surveyor spacecraft successfully orbited Mars for over nine Earth years, its instruments returning a plethora of data that still today form important, key data sets in Mars research. A relatively underutilized data set was returned from the Mars Orbiter Camera (MOC), specifically the wide‐angle component (MOC‐WA), despite returning over 150,000 images in “blue” and “red” wavelengths. The median imaging time of day was 14:00, resulting in few shadows, making it difficult to use for geology, while better cameras arrived within a few years. However, the limb‐to‐limb coverage of the MOC‐WA survey images provides an important resource, where the imaging time that was poor for geology is good for measuring reflectivity. To‐date, the only published albedo maps of Mars are from a companion MGS instrument, TES, with wide wavelength coverage and low spatial resolution, and the OMEGA instrument on Mars Express . Modern processing of the MOC‐WA images, presented here, allow for the creation of new reflectivity maps in a narrow wavelength range that can be used for photometric control of other data sets and understanding broad‐scale surface changes on Mars. Four reflectivity maps were made, at cardinal L s points, averaging images taken within just a week of each L s but across multiple Mars years. From these maps, several trends are revealed though most have been previously described, including significant differences in seasonal frost cover surrounding each residual polar ice cap, and significant changes across Syrtis Major, Solis Lacus, and the Tharsis volcanoes.