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- W2334697120 abstract "Introduction: Distinctive layers are observed exposed on the walls of troughs and scarps at the north and south polar deposits on Mars. Formation theories regard the layers as products of climate change due to orbital cycles [1, 2, 3], similar to climate changes caused by Milankovitch cycles on Earth [4], although the details of the formation processes remain unknown. Recent analyses of the north polar layered deposits (NPLD) have taken the first steps in unraveling the polar stratigraphic record and the relationship between the layers and climate [5, 6, 7]. The south polar layered deposits (SPLD), while differing morphologically from those of the north, are also thought to record the signals of a changing climate. Here we adapt the techniques of [6, 7] to an analysis of the SPLD using Mars Global Surveyor MOC images, MOLA topographic data, and Mars Odyssey THEMIS images. Methods: Many studies of terrestrial climate change are in the field of paleoceanography. We use two techniques commonly employed in paleoceanography for the study of deep-sea sediment cores on Earth to establish the characteristics of layers in individual cores (Fourier analysis) and to determine the correlation between cores (curve-shape matching algorithms). By applying these methods to study the stratigraphy of the SPLD we will be able to assess patterns and correlations between locations within the deposits." @default.
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- W2334697120 date "2006-01-01" @default.
- W2334697120 modified "2023-09-26" @default.
- W2334697120 title "INITIAL RESULTS OF STRATIGRAPHIC AND SIGNAL ANALYSIS OF THE MARS SOUTH POLAR" @default.
- W2334697120 hasPublicationYear "2006" @default.
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