Observations of the J = 1-0 CO lines in the Mars atmosphere: Radiodetection of 13CO and monitoring of 12CO
dc.contributor.author | Lellouch, E. | en_US |
dc.contributor.author | Gerin, M. | en_US |
dc.contributor.author | Combes, F. | en_US |
dc.contributor.author | Atreya, Sushil K. | en_US |
dc.contributor.author | Encrenaz, Therese | en_US |
dc.date.accessioned | 2006-04-07T20:54:35Z | |
dc.date.available | 2006-04-07T20:54:35Z | |
dc.date.issued | 1989-02 | en_US |
dc.identifier.citation | Lellouch, E., Gerin, M., Combes, F., Atreya, S., Encrenaz, T. (1989/02)."Observations of the J = 1-0 CO lines in the Mars atmosphere: Radiodetection of 13CO and monitoring of 12CO." Icarus 77(2): 414-438. <http://hdl.handle.net/2027.42/28079> | en_US |
dc.identifier.uri | http://www.sciencedirect.com/science/article/B6WGF-473144R-14Y/2/7a5557414a474ff8b4f455a751abfd20 | en_US |
dc.identifier.uri | https://hdl.handle.net/2027.42/28079 | |
dc.description.abstract | Repeated millimeter-wave observations of Mars, performed in September and October 1986 and January 1987, allowed a high-resolution recording of the J = 1-0 12CO line, and the first radiodetection of 13CO. In the hypothesis where the thermal profile has the structure measured by the Viking spacecrafts, our observations are not compatible with a terrestrial 12C/13C isotopic ratio. If the isotope ratio is assumed terrestrial, then the observations imply that the thermal profile is very different from the profile in dust-free conditions, especially in its lower part, and that the CO abundance could vary by a factor of about 2 over a period of a few months. | en_US |
dc.format.extent | 1212348 bytes | |
dc.format.extent | 3118 bytes | |
dc.format.mimetype | application/pdf | |
dc.format.mimetype | text/plain | |
dc.language.iso | en_US | |
dc.publisher | Elsevier | en_US |
dc.title | Observations of the J = 1-0 CO lines in the Mars atmosphere: Radiodetection of 13CO and monitoring of 12CO | en_US |
dc.type | Article | en_US |
dc.rights.robots | IndexNoFollow | en_US |
dc.subject.hlbsecondlevel | Astronomy | en_US |
dc.subject.hlbtoplevel | Science | en_US |
dc.description.peerreviewed | Peer Reviewed | en_US |
dc.contributor.affiliationum | Department of Atmospheric, Oceanic and Space Sciences, University of Michigan, Ann Arbor, Michigan 48109-2143, USA | en_US |
dc.contributor.affiliationother | Département de Recherches Spatiales, Observatoire de Paris-Meudon, 92195, Meudon Principal Cedex, France | en_US |
dc.contributor.affiliationother | Laboratoire de Radio Astronomie Millimétrique, Ecole Normale Supérieure, 24, rue Lhomond, 75005, Paris, France | en_US |
dc.contributor.affiliationother | Laboratoire de Radio Astronomie Millimétrique, Ecole Normale Supérieure, 24, rue Lhomond, 75005, Paris, France | en_US |
dc.contributor.affiliationother | Département de Recherches Spatiales, Observatoire de Paris-Meudon, 92195, Meudon Principal Cedex, France | en_US |
dc.description.bitstreamurl | http://deepblue.lib.umich.edu/bitstream/2027.42/28079/1/0000524.pdf | en_US |
dc.identifier.doi | http://dx.doi.org/10.1016/0019-1035(89)90097-3 | en_US |
dc.identifier.source | Icarus | en_US |
dc.owningcollname | Interdisciplinary and Peer-Reviewed |
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