LRO-LAMP Observations of the Preperihelion Coma of Comet C/2013 A1 (Siding Spring)

被引:0
|
作者
Magana, Lizeth O. [1 ,2 ]
Retherford, Kurt D. [1 ,2 ]
Bodewits, Dennis [3 ]
Feaga, Lori M. [4 ]
Grava, Cesare [2 ]
Feldman, Paul D. [5 ]
Greathouse, Thomas K. [2 ]
Noonan, John W. [6 ]
机构
[1] Univ Texas San Antonio, Dept Phys & Astron, San Antonio, TX 78249 USA
[2] Southwest Res Inst, Space Sci & Engn Dept, San Antonio, TX 78238 USA
[3] Auburn Univ, Leach Sci Ctr, Phys Dept, Auburn, AL 36849 USA
[4] Univ Maryland, College Pk, MD 20742 USA
[5] Johns Hopkins Univ, Baltimore, MD 21218 USA
[6] Univ Arizona, Lunar & Planetary Lab, Tucson, AZ 85721 USA
来源
PLANETARY SCIENCE JOURNAL | 2022年 / 3卷 / 01期
关键词
RATES; SOLAR;
D O I
10.3847/PSJ/ac3fa5
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
The Lyman-Alpha Mapping Project (LAMP) UV spectrograph on board the Lunar Reconnaissance Orbiter observed comet C/2013 A1 (Siding Spring) from lunar orbit at closest approach. On 2014 September 5, Siding Spring came within similar to 0.89 au of the Earth-Moon system and provided an opportunity for LAMP to contribute to the broader campaign of observations. The comet coma was imaged during two consecutive orbits, approximately 2 hr apart. Coma emissions of atomic oxygen were resolved within LAMP observations at distances up to similar to 1.4 x 10(6) km from the comet nucleus. We report an atomic production rate for the observed oxygen of 9.42 +/- 0.22 x 10(27) s(-1). We additionally place upper limits on the column densities of candidate species including noble gases and primary transitions. Leveraging this, we place upper limits on the production of hydrogen and carbon of <3.59 x 10(26) s(-1) and <8.41 x 10(25) s(-1), respectively. Additionally, we derive OH and H2O production rates and estimate an upper limit on the production of CO. The H2O (8.17 +/- 2.64 x 10(27) s(-1)) and OH (7.53 +/- 2.244 x 10(27) s(-1)) production rates are found to be in general agreement with previous studies when production rates are derived utilizing oxygen observations, branching ratios, and empirical formulations. Similarly, the upper limit on the production of CO (<1.33 x 10(28) s(-1)) is found to be in good agreement with previous studies (within similar to 10%) when we utilize the upper limit on CO Fourth Positive group emissions.
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页数:9
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