The Mastcam‐Z Radiometric Calibration Targets on NASA's Perseverance Rover: Derived Irradiance Time‐Series, Dust Deposition, and Performance Over the First 350 Sols on Mars
Abstract:The Mastcam‐Z radiometric calibration targets mounted on the NASA's Perseverance rover proved to be effective in the calibration of Mastcam‐Z images to reflectance (I/F) over the first 350 sols on Mars. Mastcam‐Z imaged the calibration targets regularly to perform reflectance calibration on multispectral image sets of targets on the Martian surface. For each calibration target image, mean radiance values were extracted for 41 distinct regions of the targets, including patches of color and grayscale materials. … Show more
“…However, unlike the typical dust‐coated rocks or soils, the VIS spectra exhibit only a weak 0.545 μm band and a positive 0.75–0.84 μm spectral slope. Merusi (2022) provide additional multispectral observations of the magnetic dust using Mastcam‐Z data (0.44–1.02 μm). In the IRS data, no clear absorption was observed in the near‐infrared range (Figure 4e).…”
The Perseverance rover, Mars 2020 mission, landed on the surface of the Jezero Crater, on February, 18 th 2021. This Martian crater is suspected to have hosted a paleolake as evidenced by the numerous detections of aqueously-altered phases and thus is a promising candidate for the search for past Martian life. The SuperCam instrument, elaborated by a consortium of American and European laboratories, plays a leading role in this investigation thanks to its highly versatile payload providing rapid, synergistic, fine-scale mineralogy, chemistry, and color imaging. After its landing, the first measurements of Martian targets with the infrared spectrometer of SuperCam (IRS) showed new instrumental behaviors that had to be characterized and calibrated to derive unbiased science data. The IRS radiometric response has thus been calibrated using periodic observations of the Aluwhite SuperCam Calibration Target (SCCT). Parasitic effects were understood and mitigated, and the instrumental dark and noise are characterized and modeled. The reflectance calibrated data products, provided periodically on the NASA Planetary Data System, are corrected from the main instrumental features.
“…However, unlike the typical dust‐coated rocks or soils, the VIS spectra exhibit only a weak 0.545 μm band and a positive 0.75–0.84 μm spectral slope. Merusi (2022) provide additional multispectral observations of the magnetic dust using Mastcam‐Z data (0.44–1.02 μm). In the IRS data, no clear absorption was observed in the near‐infrared range (Figure 4e).…”
The Perseverance rover, Mars 2020 mission, landed on the surface of the Jezero Crater, on February, 18 th 2021. This Martian crater is suspected to have hosted a paleolake as evidenced by the numerous detections of aqueously-altered phases and thus is a promising candidate for the search for past Martian life. The SuperCam instrument, elaborated by a consortium of American and European laboratories, plays a leading role in this investigation thanks to its highly versatile payload providing rapid, synergistic, fine-scale mineralogy, chemistry, and color imaging. After its landing, the first measurements of Martian targets with the infrared spectrometer of SuperCam (IRS) showed new instrumental behaviors that had to be characterized and calibrated to derive unbiased science data. The IRS radiometric response has thus been calibrated using periodic observations of the Aluwhite SuperCam Calibration Target (SCCT). Parasitic effects were understood and mitigated, and the instrumental dark and noise are characterized and modeled. The reflectance calibrated data products, provided periodically on the NASA Planetary Data System, are corrected from the main instrumental features.
“…We note that these values are estimates: the surface is not homogeneous, which allows for large amounts of dust to remain within coarse sands after dust removal events (Greeley et al., 2005; Reiss et al., 2010) and there are albedo spatial variations (albedo changes due to dust removal are difficult to observe on surfaces with similar reflectance such as optically thick dust layers). Furthermore, two‐layer radiative transfer models of dust‐coated surfaces reveal the strong dependence of illumination and observation angles on constraining dust thickness (Johnson, Sohl‐Dickstein, et al., 2006; Johnson et al., 2003, 2004, Kinch et al., 2007, 2015; Merusi et al., 2022), which has not been considered fully here.…”
Section: Overall Discussionmentioning
confidence: 99%
“…These observations allow the identification of albedo changes by comparing images of the same target acquired under very similar conditions. In addition, they provide information on the spectral reflectance using the blue, green and red Bayer filters, characterized by effective wavelengths of 480, 544, and 630 nm (respectively) and half‐width at half‐maximum values between 41 and 46 nm (Bell et al., 2021; Merusi et al., 2022). From these three reflectance values it is possible to calculate the green Bayer filter band depth in a way analogous to Jacob et al.…”
The Martian atmosphere interacts with the surface, redistributing dust and sand particles (Kahre et al., 2017). Small particles are lifted by convective vortices and by strong wind gusts, and are subsequently transported before settling again (
“…(2020) and Merusi et al. (2022). Additional details about the software tools developed for multispectral data processing tasks can be found in Million et al.…”
Section: Instrumentation and Methodsmentioning
confidence: 95%
“…Variance bars indicate the standard deviation of reflectance values from those pixels on each filter's associated image that fall within the specific region of interest (ROI). Details about the Mastcam-Z onboard calibration targets and their use in generating reflectance factor data can be found in Kinch et al (2020) and Merusi et al (2022). Additional details about the software tools developed for multispectral data processing tasks can be found in Million et al (2022).…”
A multi‐instrument study of the regolith of Jezero crater floor units by the Perseverance rover has identified three types of regolith: fine‐grained, coarse‐grained, and mixed‐type. Mastcam‐Z, Wide Angle Topographic Sensor for Operations and eNgineering, and SuperCam Remote Micro Imager were used to characterize the regolith texture, particle size, and roundedness where possible. Mastcam‐Z multispectral and SuperCam laser‐induced breakdown spectroscopy data were used to constrain the composition of the regolith types. Fine‐grained regolith is found surrounding bedrock and boulders, comprising bedforms, and accumulating on top of rocks in erosional depressions. Spectral and chemical data show it is compositionally consistent with pyroxene and a ferric‐oxide phase. Coarse‐grained regolith consists of 1–2 mm well‐sorted gray grains that are found concentrated around the base of boulders and bedrock, and armoring bedforms. Its chemistry and spectra indicate it is olivine‐bearing, and its spatial distribution and roundedness indicate it has been transported, likely by saltation‐induced creep. Coarse grains share similarities with the olivine grains observed in the Séítah formation bedrock, making that unit a possible source for these grains. Mixed‐type regolith contains fine‐ and coarse‐grained regolith components and larger rock fragments. The rock fragments are texturally and spectrally similar to bedrock within the Máaz and Séítah formations, indicating origins by erosion from those units, although they could also be a lag deposit from erosion of an overlying unit. The fine‐ and coarse‐grained types are compared to their counterparts at other landing sites to inform global, regional, and local inputs to regolith formation within Jezero crater. The regolith characterization presented here informs the regolith sampling efforts underway by Perseverance.
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