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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Published in:Science
Main Authors: Slade, Martin A., Butler, Bryan J., Muhleman, Duane O.
Format: Article in Journal/Newspaper
Language:English
Published: American Association for the Advancement of Science (AAAS) 1992
Subjects:
Online Access:http://dx.doi.org/10.1126/science.258.5082.635
https://www.science.org/doi/pdf/10.1126/science.258.5082.635
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spelling craaas:10.1126/science.258.5082.635 2024-06-23T07:55:24+00:00 Mercury Radar Imaging: Evidence for Polar Ice Slade, Martin A. Butler, Bryan J. Muhleman, Duane O. 1992 http://dx.doi.org/10.1126/science.258.5082.635 https://www.science.org/doi/pdf/10.1126/science.258.5082.635 en eng American Association for the Advancement of Science (AAAS) Science volume 258, issue 5082, page 635-640 ISSN 0036-8075 1095-9203 journal-article 1992 craaas https://doi.org/10.1126/science.258.5082.635 2024-06-13T04:01:14Z 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 (μ c ) was 1.0 to 1.4; values < ∼0.1 are typical for terrestrial planets. Such high values of μ c have hitherto been observed in radar observations only from icy regions of Mars and icy outer planet satellites. Article in Journal/Newspaper North Pole AAAS Resource Center (American Association for the Advancement of Science) North Pole Science 258 5082 635 640
institution Open Polar
collection AAAS Resource Center (American Association for the Advancement of Science)
op_collection_id craaas
language English
description 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 (μ c ) was 1.0 to 1.4; values < ∼0.1 are typical for terrestrial planets. Such high values of μ c have hitherto been observed in radar observations only from icy regions of Mars and icy outer planet satellites.
format Article in Journal/Newspaper
author Slade, Martin A.
Butler, Bryan J.
Muhleman, Duane O.
spellingShingle Slade, Martin A.
Butler, Bryan J.
Muhleman, Duane O.
Mercury Radar Imaging: Evidence for Polar Ice
author_facet Slade, Martin A.
Butler, Bryan J.
Muhleman, Duane O.
author_sort Slade, Martin A.
title Mercury Radar Imaging: Evidence for Polar Ice
title_short Mercury Radar Imaging: Evidence for Polar Ice
title_full Mercury Radar Imaging: Evidence for Polar Ice
title_fullStr Mercury Radar Imaging: Evidence for Polar Ice
title_full_unstemmed Mercury Radar Imaging: Evidence for Polar Ice
title_sort mercury radar imaging: evidence for polar ice
publisher American Association for the Advancement of Science (AAAS)
publishDate 1992
url http://dx.doi.org/10.1126/science.258.5082.635
https://www.science.org/doi/pdf/10.1126/science.258.5082.635
geographic North Pole
geographic_facet North Pole
genre North Pole
genre_facet North Pole
op_source Science
volume 258, issue 5082, page 635-640
ISSN 0036-8075 1095-9203
op_doi https://doi.org/10.1126/science.258.5082.635
container_title Science
container_volume 258
container_issue 5082
container_start_page 635
op_container_end_page 640
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