Araki, H. and Tazawa, S. and Noda, H. and Ishihara, Y. and Goossens, S. and Sasaki, S. and Kawano, N. and Kamiya, I. and Otake, H. and Oberst, J. and Shum, C. (2009) Lunar Global Shape and Polar Topography Derived from Kaguya-LALT Laser Altimetry. Science, 323, pp. 897-900. American Association for the Advancement of Science. DOI: 10.1126/science.1164146. ISSN 1095-9203.
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Official URL: http://www.sciencemag.org
A global lunar topographic map with a spatial resolution of finer than 0.5 degree has been derived using data from the laser altimeter (LALT) on board the Japanese lunar explorer Selenological and Engineering Explorer (SELENE or Kaguya). In comparison with the previous Unified Lunar Control Network (ULCN 2005) model, the new map reveals unbiased lunar topography for scales finer than a few hundred kilometers. Spherical harmonic analysis of global topographic data for the Moon, Earth, Mars, and Venus suggests that isostatic compensation is the prevailing lithospheric support mechanism at large scales. However, simple rigid support is suggested to dominate for the Moon, Venus, and Mars for smaller scales, which may indicate a drier lithosphere than on Earth, especially for the Moon and Venus.
|Title:||Lunar Global Shape and Polar Topography Derived from Kaguya-LALT Laser Altimetry|
|Date:||13 February 2009|
|Journal or Publication Title:||Science|
|In Open Access:||No|
|In ISI Web of Science:||Yes|
|Page Range:||pp. 897-900|
|Publisher:||American Association for the Advancement of Science|
|Keywords:||Moon, Laser Altimetry, Kaguya, LALT|
|HGF - Research field:||Aeronautics, Space and Transport (old)|
|HGF - Program:||Space (old)|
|HGF - Program Themes:||W EW - Erforschung des Weltraums|
|DLR - Research area:||Space|
|DLR - Program:||W EW - Erforschung des Weltraums|
|DLR - Research theme (Project):||W - Vorhaben Vergleichende Planetologie (old)|
|Institutes and Institutions:||Institute of Planetary Research > Planetary Geodesy|
|Deposited By:||Marita Wählisch|
|Deposited On:||08 Dec 2009 08:29|
|Last Modified:||07 Feb 2013 20:42|
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