Infrared scans of Saturn
Scans are presented at five wavelengths between 7.8 and 25 microns north-south along Saturn's central meridian and east-west parallel to the equator through the subearth point. The brightening of Saturn's South Pole at 12.7 microns was more enhanced in 1977 than in 1978 due to the 5 deg gr...
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ftnasantrs:oai:casi.ntrs.nasa.gov:19800058155 2023-05-15T18:22:09+02:00 Infrared scans of Saturn Sinton, W. M. Macy, W. W. Good, J. Orton, G. S. Unclassified, Unlimited, Publicly available May 1, 1980 http://ntrs.nasa.gov/search.jsp?R=19800058155 unknown http://ntrs.nasa.gov/search.jsp?R=19800058155 Accession ID: 80A42325 Copyright Other Sources 91 Icarus; 42; May 1980 1980 ftnasantrs 2012-02-15T14:22:02Z Scans are presented at five wavelengths between 7.8 and 25 microns north-south along Saturn's central meridian and east-west parallel to the equator through the subearth point. The brightening of Saturn's South Pole at 12.7 microns was more enhanced in 1977 than in 1978 due to the 5 deg greater declination of the polar axis in 1977. There is a plateau in the Southern Hemisphere between -30 and -60 deg latitude in the 7.8 and 12.7 micron scans. The apparent temperature of the rings decreased as Saturn approached the equinox. It is found generally that the strongest ring emission arises from the C ring. Other/Unknown Material South pole NASA Technical Reports Server (NTRS) South Pole |
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Open Polar |
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NASA Technical Reports Server (NTRS) |
op_collection_id |
ftnasantrs |
language |
unknown |
topic |
91 |
spellingShingle |
91 Sinton, W. M. Macy, W. W. Good, J. Orton, G. S. Infrared scans of Saturn |
topic_facet |
91 |
description |
Scans are presented at five wavelengths between 7.8 and 25 microns north-south along Saturn's central meridian and east-west parallel to the equator through the subearth point. The brightening of Saturn's South Pole at 12.7 microns was more enhanced in 1977 than in 1978 due to the 5 deg greater declination of the polar axis in 1977. There is a plateau in the Southern Hemisphere between -30 and -60 deg latitude in the 7.8 and 12.7 micron scans. The apparent temperature of the rings decreased as Saturn approached the equinox. It is found generally that the strongest ring emission arises from the C ring. |
format |
Other/Unknown Material |
author |
Sinton, W. M. Macy, W. W. Good, J. Orton, G. S. |
author_facet |
Sinton, W. M. Macy, W. W. Good, J. Orton, G. S. |
author_sort |
Sinton, W. M. |
title |
Infrared scans of Saturn |
title_short |
Infrared scans of Saturn |
title_full |
Infrared scans of Saturn |
title_fullStr |
Infrared scans of Saturn |
title_full_unstemmed |
Infrared scans of Saturn |
title_sort |
infrared scans of saturn |
publishDate |
1980 |
url |
http://ntrs.nasa.gov/search.jsp?R=19800058155 |
op_coverage |
Unclassified, Unlimited, Publicly available |
geographic |
South Pole |
geographic_facet |
South Pole |
genre |
South pole |
genre_facet |
South pole |
op_source |
Other Sources |
op_relation |
http://ntrs.nasa.gov/search.jsp?R=19800058155 Accession ID: 80A42325 |
op_rights |
Copyright |
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1766201524338294784 |