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Conference Paper: Radio monitoring of 9P/tempel 1 outgassing and gas released by the impact
Title | Radio monitoring of 9P/tempel 1 outgassing and gas released by the impact |
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Authors | |
Issue Date | 2009 |
Citation | Eso Astrophysics Symposia, 2009, v. 2009, p. 233-241 How to Cite? |
Abstract | As part of the international observing campaign in support of the NASA Deep Impact mission to comet 9P/Tempel 1, we conducted a monitoring of its outgassing at radio wavelengths. OH observations conducted at the Nançay radio telescope provided a 4-month monitoring of the comet from March to July, followed by the observation of H 2O with the Odin satellite from June to August 2005. The peak of outgassing was found to be around 10 28 molec. s -1 between May and July. Observations of HCN conducted with the IRAM 30 m radio telescope in May 2005 showed a variation of the production rate with a period of 1.73±0.10 days, consistent with the rotation period of the nucleus. The Odin satellite also monitored nearly continuously the H 2O line at 557 GHz during the 38 h following the impact on the 4th of July. Once possible periodic variations related to the nucleus rotation are removed, a small increase of outgassing related to the impact is present, which corresponds to the release of 5000±2000 tons of water. Two other bursts of activity were seen on 23 June and 7 July. ©2009 Springer-Verlag Berlin Heidelberg. |
Persistent Identifier | http://hdl.handle.net/10722/179625 |
ISSN | |
ISI Accession Number ID | |
References |
DC Field | Value | Language |
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dc.contributor.author | Biver, N | en_US |
dc.contributor.author | BockeléeMorvan, D | en_US |
dc.contributor.author | Boissier, J | en_US |
dc.contributor.author | Crovisier, J | en_US |
dc.contributor.author | Colom, P | en_US |
dc.contributor.author | Lecacheux, A | en_US |
dc.contributor.author | Moreno, R | en_US |
dc.contributor.author | Paubert, G | en_US |
dc.contributor.author | Lis, DC | en_US |
dc.contributor.author | Sumner, M | en_US |
dc.contributor.author | Frisk, U | en_US |
dc.contributor.author | Hjalmarson, Å | en_US |
dc.contributor.author | Olberg, M | en_US |
dc.contributor.author | Winnberg, A | en_US |
dc.contributor.author | Florén, H | en_US |
dc.contributor.author | Sandqvist, A | en_US |
dc.contributor.author | Kwok, S | en_US |
dc.date.accessioned | 2012-12-19T10:01:42Z | - |
dc.date.available | 2012-12-19T10:01:42Z | - |
dc.date.issued | 2009 | en_US |
dc.identifier.citation | Eso Astrophysics Symposia, 2009, v. 2009, p. 233-241 | en_US |
dc.identifier.issn | 1431-2433 | en_US |
dc.identifier.uri | http://hdl.handle.net/10722/179625 | - |
dc.description.abstract | As part of the international observing campaign in support of the NASA Deep Impact mission to comet 9P/Tempel 1, we conducted a monitoring of its outgassing at radio wavelengths. OH observations conducted at the Nançay radio telescope provided a 4-month monitoring of the comet from March to July, followed by the observation of H 2O with the Odin satellite from June to August 2005. The peak of outgassing was found to be around 10 28 molec. s -1 between May and July. Observations of HCN conducted with the IRAM 30 m radio telescope in May 2005 showed a variation of the production rate with a period of 1.73±0.10 days, consistent with the rotation period of the nucleus. The Odin satellite also monitored nearly continuously the H 2O line at 557 GHz during the 38 h following the impact on the 4th of July. Once possible periodic variations related to the nucleus rotation are removed, a small increase of outgassing related to the impact is present, which corresponds to the release of 5000±2000 tons of water. Two other bursts of activity were seen on 23 June and 7 July. ©2009 Springer-Verlag Berlin Heidelberg. | en_US |
dc.language | eng | en_US |
dc.relation.ispartof | ESO Astrophysics Symposia | en_US |
dc.title | Radio monitoring of 9P/tempel 1 outgassing and gas released by the impact | en_US |
dc.type | Conference_Paper | en_US |
dc.identifier.email | Kwok, S: deannote@hku.hk | en_US |
dc.identifier.authority | Kwok, S=rp00716 | en_US |
dc.description.nature | link_to_subscribed_fulltext | en_US |
dc.identifier.doi | 10.1007/978-3-540-76959-0_31 | en_US |
dc.identifier.scopus | eid_2-s2.0-54849430002 | en_US |
dc.relation.references | http://www.scopus.com/mlt/select.url?eid=2-s2.0-54849430002&selection=ref&src=s&origin=recordpage | en_US |
dc.identifier.volume | 2009 | en_US |
dc.identifier.spage | 233 | en_US |
dc.identifier.epage | 241 | en_US |
dc.identifier.isi | WOS:000262404900031 | - |
dc.publisher.place | Germany | en_US |
dc.identifier.scopusauthorid | Biver, N=6603734959 | en_US |
dc.identifier.scopusauthorid | BockeléeMorvan, D=7003530700 | en_US |
dc.identifier.scopusauthorid | Boissier, J=7101971162 | en_US |
dc.identifier.scopusauthorid | Crovisier, J=35448565400 | en_US |
dc.identifier.scopusauthorid | Colom, P=6603805418 | en_US |
dc.identifier.scopusauthorid | Lecacheux, A=7003423533 | en_US |
dc.identifier.scopusauthorid | Moreno, R=7202177731 | en_US |
dc.identifier.scopusauthorid | Paubert, G=6701489710 | en_US |
dc.identifier.scopusauthorid | Lis, DC=7005226300 | en_US |
dc.identifier.scopusauthorid | Sumner, M=10638914800 | en_US |
dc.identifier.scopusauthorid | Frisk, U=8966521600 | en_US |
dc.identifier.scopusauthorid | Hjalmarson, Å=15744175200 | en_US |
dc.identifier.scopusauthorid | Olberg, M=16201342800 | en_US |
dc.identifier.scopusauthorid | Winnberg, A=6603734778 | en_US |
dc.identifier.scopusauthorid | Florén, H=6602447564 | en_US |
dc.identifier.scopusauthorid | Sandqvist, A=35451841800 | en_US |
dc.identifier.scopusauthorid | Kwok, S=22980498300 | en_US |
dc.identifier.issnl | 1431-2433 | - |