Mercury Radar Imaging: Evidence for Polar Ice

The first unambiguous full-disk radar mapping of Mercury at 3.5-centimeter wavelength, with the Goldstone 70-meter antenna transmitting and 26 antennas of the Very Large Array receiving, has provided evidence for the presence of polar ice. The radar experiments, conducted on 8 and 23 August 1991, we...

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Bibliographic Details
Published in:Science
Main Authors: Slade, Martin A., Butler, Bryan J., Muhleman, Duane O.
Format: Article in Journal/Newspaper
Language:unknown
Published: American Association for the Advancement of Science 1992
Subjects:
Online Access:https://authors.library.caltech.edu/53999/
https://resolver.caltech.edu/CaltechAUTHORS:20150122-132953915
Description
Summary:The first unambiguous full-disk radar mapping of Mercury at 3.5-centimeter wavelength, with the Goldstone 70-meter antenna transmitting and 26 antennas of the Very Large Array receiving, has provided evidence for the presence of polar ice. The radar experiments, conducted on 8 and 23 August 1991, were designed to image the half of Mercury not photographed by Mariner 10. The orbital geometry allowed viewing beyond the north pole of Mercury; a highly reflective region was clearly visible on the north pole during both experiments. This polar region has areas in which the circular polarization ratio (pt) was 1.0 to 1.4; values <∼0.1 are typical for terrestrial planets. Such high values of have hitherto been observed in radar observations only from icy regions of Mars and icy outer planet satellites.