4.3 Article

LU60645GT and MA132843GT catalogues of Lunar and Martian impact craters developed using a Crater Shape-based interpolation crater detection algorithm for topography data

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PLANETARY AND SPACE SCIENCE
卷 60, 期 1, 页码 236-247

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PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.pss.2011.09.003

关键词

Moon; Mars; Surface; Cratering; Image processing

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For Mars, 57,633 craters from the manually assembled catalogues and 72,668 additional craters identified using several crater detection algorithms (CDAs) have been merged into the MA130301GT catalogue. By contrast, for the Moon the most complete previous catalogue contains only 74,923 craters. Two recent missions provided higher-quality digital elevation maps (DEMs): SELENE (in 1/16 degrees resolution) and Lunar Reconnaissance Orbiter (we used up to 1/512 degrees). This was the main motivation for work on the new Crater Shape-based interpolation module, which improves previous CDA as follows: (1) it decreases the number of false-detections for the required number of true detections; (2) it improves detection capabilities for very small craters; and (3) it provides more accurate automated measurements of craters' properties. The results are: (1) LU60645GT, which is currently the most complete (up to similar to D >= 8 km) catalogue of Lunar craters; and (2) MA132843GT catalogue of Martian craters complete up to similar to D >= 2 km, which is the extension of the previous MA130301GT catalogue. As previously achieved for Mars, LU60645GT provides all properties that were provided by the previous Lunar catalogues, plus: (1) correlation between morphological descriptors from used catalogues; (2) correlation between manually assigned attributes and automated measurements; (3) average errors and their standard deviations for manually and automatically assigned attributes such as position coordinates, diameter, depth/diameter ratio, etc; and (4) a review of positional accuracy of used datasets. Additionally, surface dating could potentially be improved with the exhaustiveness of this new catalogue. The accompanying results are: (1) the possibility of comparing a large number of Lunar and Martian craters, of e.g. depth/diameter ratio and 2D profiles; (2) utilisation of a method for re-projection of datasets and catalogues, which is very useful for craters that are very close to poles; and (3) the extension of the previous framework for evaluation of CDAs with datasets and ground-truth catalogue for the Moon. (C) 2011 Elsevier Ltd. All rights reserved.

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