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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American Association for the Advancement of Science
1976
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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 |
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Caltech Authors (California Institute of Technology) |
op_collection_id |
ftcaltechauth |
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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 resolverid:CaltechAUTHORS:20170227-162205245 |
op_rights |
info:eu-repo/semantics/closedAccess Other |
op_doi |
https://doi.org/10.1126/science.193.4255.780 |
container_title |
Science |
container_volume |
193 |
container_issue |
4255 |
container_start_page |
780 |
op_container_end_page |
786 |
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1802649334438690816 |