Measurement of the meteoroid flux at Mars

被引:22
作者
Domokos, A. [1 ]
Bell, J. F., III
Brown, P.
Lemmon, M. T.
Suggs, R.
Vaubaillon, J.
Cooke, W.
机构
[1] Univ Western Ontario, Dept Phys & Astron, London, ON N6A 3K7, Canada
[2] Cornell Univ, Dept Astron, Ithaca, NY 14853 USA
[3] Texas A&M Univ, Dept Atmospher Sci, College Stn, TX 77843 USA
[4] NASA, George C Marshall Space Flight Ctr, Space Environm Team EV13, Meteoriod Environm Off, Huntsville, AL 35812 USA
[5] CALTECH, Spitzer Sci Ctr, Pasadena, CA 91125 USA
基金
加拿大自然科学与工程研究理事会; 美国国家航空航天局;
关键词
cosmic rays; image processing; instrumentation;
D O I
10.1016/j.icarus.2007.04.017
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
In the fall of 2005, a dedicated meteor observing campaign was carried out by the Panoramic Camera (Pancam) onboard the Mars Exploration Rover (MER) Spirit to determine the viability of using MER cameras as meteor detectors and to obtain the first experimental estimate of the meteoroid flux at Mars. Our observing targets included both the sporadic meteoroid background and two predicted martian meteor showers: one associated with IP/Halley and a potential stream associated with 2001/R1 LONEOS. A total of 353 images covering 2.7 h of net exposure time were analyzed with no conclusive meteor detections. From these data, an upper limit to the background meteoroid flux at Mars is estimated to be <4.4 x 10(-6) meteoroids km(-2) h(-1) for meteoroids with mass larger than 4 g. For comparison, the estimated flux to this mass limit at the Earth is 10-6 meteoroids km-2 h- 1 [Grun, E., Zook, H.A., Fechtiig, H., Giese, R.H., 1985. Icarus 62, 244-272]. This result is qualitatively consistent, within error bounds, with theoretical models predicting martian fluxes of similar to 50% that at Earth for meteoroids of mass 10(-3)-10(1) g [Adolfsson, L.G., Gustafson, B.A.S., Murray, C.D., 1996. Icarus 119, 144-152]. The MER cameras, even using the most sensitive mode of operation, should expect to see on average only one coincident meteor on of order 40-150 It of total exposure time based on these same theoretical martian flux estimates. To more meaningfully constrain these flux models, a longer total integrated exposure time or more sensitive camera is needed. Our analysis also suggests that the event reported as the first martian meteor [Selsis, F., Lemmon, M.T., Vaubaillon, J., Bell, U., 2005. Nature 435, 5811 is more likely a grazing cosmic ray impact, which we show to be a major source of confusion with potential meteors in all Pancam images. (C) 2007 Elsevier Inc. All rights reserved.
引用
收藏
页码:141 / 150
页数:10
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