The shape of Mars before Global Surveyor: Results from reanalysis of the Viking control point network

Zeitler, W.; Oberst, J.

doi:10.1029/1999je900011

Cited by 2 publications

(1 citation statement)

References 19 publications

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“…Because the Mars Global Surveyor spacecraft positioning is much more precise than that of the Viking Orbiters, measured elevations differ significantly from elevations from the Viking missions. We find the MOLA elevations are 775 m lower than Viking stereogrammetric elevations, well within the observed 1-2 km difference between MOLA elevations and the Viking DTM (Zeitler andOberst 1999, Smith et al 1998).…”

Section: Mola Resultssupporting

confidence: 73%

Topography and Stratigraphy of the Northern Martian Polar Layered Deposits Using Photoclinometry, Stereogrammetry, and MOLA Altimetry

Fenton

Herkenhoff

2000

Icarus

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Section: Mola Resultssupporting

confidence: 73%

Topography and Stratigraphy of the Northern Martian Polar Layered Deposits Using Photoclinometry, Stereogrammetry, and MOLA Altimetry

Fenton

Herkenhoff

2000

Icarus

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High‐resolution digital elevation models derived from Viking Orbiter images: Method and comparison with Mars Orbiter Laser Altimeter Data

Baratoux¹,

Delacourt²,

Allemand³

2001

J. Geophys. Res.

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The purpose of this paper is to present a method to derive local and high‐resolution digital elevation models (DEM) of Mars from Viking Orbiter images. We focus on two aspects that appear to be new in photogrammetry applied to Mars: the correlation method and the relative orientation method based on the analysis of the coplaneity. We demonstrate that a DEM from two Viking Orbiter images selected according to the criteria of parallax height ratio, resolution, and illumination conditions can be obtained with a better spatial lateral resolution than the interpolated Mars Orbiter Laser Altimeter (MOLA) data. Two images on the Deuteronilus Mensae area satisfy these criteria. The algorithm of reconstruction of the topography is divided into two steps. First, a correlation method at subpixel level based on Fourier transform has been adapted to extract image location of homologous points. As initial camera positions and angles are known with poor accuracy, an adjustment is then carried out by the method of relative orientation which requires no absolute control points and takes advantage of the subpixel accuracy of our matching algorithm. Finally, the DEM is projected into a Martian reference frame and registered to MOLA data for validation. The spatial resolution depends on the roughness of the area and is locally close to the distance between individual MOLA footprints along one profile (300 m), as demonstrated from the comparison with MOLA profiles. These first results of high‐resolution DEM from Viking Orbiter images should be used with MOLA data for many geological studies that require high‐resolution topographic data.

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The shape of Mars before Global Surveyor: Results from reanalysis of the Viking control point network

Abstract: Abstract.Three-dimensional coordinates of 3739 globally distributed control points derived from photogrammetric analysis of Viking Orbiter image data are studied with respect to the shape and large-scale morphology of Mars.

Cited by 2 publications

References 19 publications

Topography and Stratigraphy of the Northern Martian Polar Layered Deposits Using Photoclinometry, Stereogrammetry, and MOLA Altimetry

Topography and Stratigraphy of the Northern Martian Polar Layered Deposits Using Photoclinometry, Stereogrammetry, and MOLA Altimetry

High‐resolution digital elevation models derived from Viking Orbiter images: Method and comparison with Mars Orbiter Laser Altimeter Data

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