Mosaicking of global planetary image datasets: 1. Techniques and data processing for Thermal Emission Imaging System (THEMIS) multi-spectral data

Christopher S. Edwards, K. Nowicki, P. R. Christensen, J. R. Hill, Noel Gorelick, K. Murray

Journal of Geophysical Research Atmospheres · 2011 · 298 citations · 65 references

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TL;DR

Mosaicking global planetary datasets enables examination of processes at multiple scales across all planetary bodies, and techniques originally developed for THEMIS infrared multispectral data—such as non‑uniformity correction, contrast stretching, and noise removal—can be adapted to other datasets, allowing diverse perspectives on composition, thermophysics, and morphology. Processing techniques that allow creation of mosaics from tens of thousands of images are documented, including image registration, blending, normalization, and error analysis; these methods are applied to generate THEMIS daytime/nighttime infrared, Viking, CTX, and MOC visible mosaics across various scales. The authors present THEMIS daytime and nighttime relative temperature global mosaics, the highest‑resolution (100 m/pixel) global‑scale data sets for Mars to date.

Abstract

[1] The mosaicking of global planetary data sets allows for the examination of local, regional, and global scale processes on all planetary bodies. Processing techniques that allow us and other users to crate mosaics of tens of thousands of images are documented along with the associated errors introduced by each image-processing algorithm. These techniques (e.g., non-uniformity correction, running contrast stretches, line and row correlated noise removal, and random noise removal) were originally developed for the 2001 Mars Odyssey Thermal Emission Imaging System (THEMIS) infrared multispectral imager data but can be adapted and applied to other data sets by the alteration of input parameters. The techniques for mosaicking planetary image data sets (e.g., image registration, blending, and normalization) are also presented along with the generation of qualitative and quantitative products. These techniques are then applied to generate THEMIS daytime and nighttime infrared, Viking, Context Imager (CTX), and Mars Orbiter Camera (MOC) visible mosaics using a variety of input and output types at a variety of scales. By creating mosaics of the same area using different data sets such as those that illustrate compositional diversity, thermophysical properties, or small-scale morphology, it is possible to view the surface of the planet and geologic problems through many different perspectives. In addition to the techniques used to create large-scale seamless mosaics, we also present the THEMIS daytime and nighttime relative temperature global mosaics, which are the highest resolution (100m/pixel) global scale data sets available for Mars to date.

References

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