Infrared Thermal Mapping of the Martian Surface and Atmosphere: First Results

The Viking infrared thermal mapper measures the thermal emission of the martian surface and atmosphere and the total reflected sunlight. With the high resolution and dense coverage being achieved, planetwide thermal structure is apparent at large and small scales. The thermal behavior of the best-ob...

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Published in:Science
Main Authors: Kieffer, Hugh H., Chase, Stillman C., Jr., Miner, Ellis D., Palluconi, Frank Don, Münch, Guido, Neugebauer, Gerry, Martin, Terry Z.
Format: Article in Journal/Newspaper
Language:unknown
Published: American Association for the Advancement of Science 1976
Subjects:
Online Access:https://doi.org/10.1126/science.193.4255.780
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spelling ftcaltechauth:oai:authors.library.caltech.edu:rw7mw-ed355 2024-06-23T07:56:19+00:00 Infrared Thermal Mapping of the Martian Surface and Atmosphere: First Results Kieffer, Hugh H. Chase, Stillman C., Jr. Miner, Ellis D. Palluconi, Frank Don Münch, Guido Neugebauer, Gerry Martin, Terry Z. 1976-08-27 https://doi.org/10.1126/science.193.4255.780 unknown American Association for the Advancement of Science oai:authors.library.caltech.edu:rw7mw-ed355 eprintid:74568 https://doi.org/10.1126/science.193.4255.780 resolverid:CaltechAUTHORS:20170227-162205245 info:eu-repo/semantics/closedAccess Other Science, 193(4255), 780-786, (1976-08-27) info:eu-repo/semantics/article 1976 ftcaltechauth https://doi.org/10.1126/science.193.4255.780 2024-06-12T02:16:01Z The Viking infrared thermal mapper measures the thermal emission of the martian surface and atmosphere and the total reflected sunlight. With the high resolution and dense coverage being achieved, planetwide thermal structure is apparent at large and small scales. The thermal behavior of the best-observed areas, the landing sites, cannot be explained by simple homogeneous models. The data contain clear indications for the relevance of additional factors such as detailed surface texture and the occurrence of clouds. Areas in the polar night have temperatures distinctly lower than the CO_2 condensation point at the surface pressure. This observation implies that the annual atmospheric condensation is less than previously assumed and that either thick CO_2 clouds exist at the 20-kilometer level or that the polar atmosphere is locally enriched by noncondensable gases. © 1976 American Association for the Advancement of Science. 26 July 1976. The two Viking IRTM experiments represent a fourfold increase in the total number of thermal detectors flown to other planets. Their success is the result of the individual efforts of a large number of people during design, fabrication, and the complex flight operations of this instrument. The prolonged efforts of Mike Agabra, Jack Engel, Howard Eyerly, Claude Michaux, Richard Ruiz, and Don Schofield are representative of this group. The massive data reduction system is a tribute to and from Bob Mehlman, John Gieselman, and Elliot Goldyn. We hope all involved take satisfaction from this evidence of their effort. Supported by Jet Propulsion Laboratory contract 952988 to the University of California. Article in Journal/Newspaper polar night Caltech Authors (California Institute of Technology) Elliot ENVELOPE(166.533,166.533,-70.883,-70.883) The Landing ENVELOPE(-45.689,-45.689,-60.733,-60.733) Science 193 4255 780 786
institution Open Polar
collection Caltech Authors (California Institute of Technology)
op_collection_id ftcaltechauth
language unknown
description The Viking infrared thermal mapper measures the thermal emission of the martian surface and atmosphere and the total reflected sunlight. With the high resolution and dense coverage being achieved, planetwide thermal structure is apparent at large and small scales. The thermal behavior of the best-observed areas, the landing sites, cannot be explained by simple homogeneous models. The data contain clear indications for the relevance of additional factors such as detailed surface texture and the occurrence of clouds. Areas in the polar night have temperatures distinctly lower than the CO_2 condensation point at the surface pressure. This observation implies that the annual atmospheric condensation is less than previously assumed and that either thick CO_2 clouds exist at the 20-kilometer level or that the polar atmosphere is locally enriched by noncondensable gases. © 1976 American Association for the Advancement of Science. 26 July 1976. The two Viking IRTM experiments represent a fourfold increase in the total number of thermal detectors flown to other planets. Their success is the result of the individual efforts of a large number of people during design, fabrication, and the complex flight operations of this instrument. The prolonged efforts of Mike Agabra, Jack Engel, Howard Eyerly, Claude Michaux, Richard Ruiz, and Don Schofield are representative of this group. The massive data reduction system is a tribute to and from Bob Mehlman, John Gieselman, and Elliot Goldyn. We hope all involved take satisfaction from this evidence of their effort. Supported by Jet Propulsion Laboratory contract 952988 to the University of California.
format Article in Journal/Newspaper
author Kieffer, Hugh H.
Chase, Stillman C., Jr.
Miner, Ellis D.
Palluconi, Frank Don
Münch, Guido
Neugebauer, Gerry
Martin, Terry Z.
spellingShingle Kieffer, Hugh H.
Chase, Stillman C., Jr.
Miner, Ellis D.
Palluconi, Frank Don
Münch, Guido
Neugebauer, Gerry
Martin, Terry Z.
Infrared Thermal Mapping of the Martian Surface and Atmosphere: First Results
author_facet Kieffer, Hugh H.
Chase, Stillman C., Jr.
Miner, Ellis D.
Palluconi, Frank Don
Münch, Guido
Neugebauer, Gerry
Martin, Terry Z.
author_sort Kieffer, Hugh H.
title Infrared Thermal Mapping of the Martian Surface and Atmosphere: First Results
title_short Infrared Thermal Mapping of the Martian Surface and Atmosphere: First Results
title_full Infrared Thermal Mapping of the Martian Surface and Atmosphere: First Results
title_fullStr Infrared Thermal Mapping of the Martian Surface and Atmosphere: First Results
title_full_unstemmed Infrared Thermal Mapping of the Martian Surface and Atmosphere: First Results
title_sort infrared thermal mapping of the martian surface and atmosphere: first results
publisher American Association for the Advancement of Science
publishDate 1976
url https://doi.org/10.1126/science.193.4255.780
long_lat ENVELOPE(166.533,166.533,-70.883,-70.883)
ENVELOPE(-45.689,-45.689,-60.733,-60.733)
geographic Elliot
The Landing
geographic_facet Elliot
The Landing
genre polar night
genre_facet polar night
op_source Science, 193(4255), 780-786, (1976-08-27)
op_relation oai:authors.library.caltech.edu:rw7mw-ed355
eprintid:74568
https://doi.org/10.1126/science.193.4255.780
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op_rights info:eu-repo/semantics/closedAccess
Other
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