Note to users. If you're seeing this message, it means that your browser cannot find this page's style/presentation instructions -- or possibly that you are using a browser that does not support current Web standards. Find out more about why this message is appearing, and what you can do to make your experience of our site the best it can be.


Science 4 June 1999:
Vol. 284. no. 5420, pp. 1658 - 1660
DOI: 10.1126/science.284.5420.1658

Reports

Topography of the Lunar Poles from Radar Interferometry: A Survey of Cold Trap Locations

J. L. Margot, 1*dagger D. B. Campbell, 1dagger R. F. Jurgens, 2 M. A. Slade 2

Detailed topographic maps of the lunar poles have been obtained by Earth-based radar interferometry with the 3.5-centimeter wavelength Goldstone Solar System Radar. The interferometer provided maps 300 kilometers by 1000 kilometers of both polar regions at 150-meter spatial resolution and 50-meter height resolution. Using ray tracing, these digital elevation models were used to locate regions that are in permanent shadow from solar illumination and may harbor ice deposits. Estimates of the total extent of shadowed areas poleward of 87.5 degrees latitude are 1030 and 2550 square kilometers for the north and south poles, respectively.

1 Department of Astronomy, Space Sciences Building, Cornell University, Ithaca, NY 14853, USA.
2 Jet Propulsion Laboratory, MS 238-420, 4800 Oak Grove Drive, Pasadena, CA 91109, USA.
*   Present address: Arecibo Observatory, HC3 Box 53995, Arecibo, PR 00612, Puerto Rico.

dagger    To whom correspondence should be addressed. E-mail: margot{at}naic.edu (J.L.M.); campbell{at}astrosun.tn.cornell.edu (D.B.C.)


Read the Full Text


THIS ARTICLE HAS BEEN CITED BY OTHER ARTICLES:
Development of the Moon.
M. B. Duke, L. R. Gaddis, G. J. Taylor, and H. H. Schmitt (2006)
Reviews in Mineralogy and Geochemistry 60, 597-655
   Full Text »    PDF »



To Advertise     Find Products


Science. ISSN 0036-8075 (print), 1095-9203 (online)