Active dust devils in Gusev crater, Mars: Observations from the Mars Exploration Rover Spirit

被引:125
|
作者
Greeley, Ronald
Whelley, Patrick L.
Arvidson, Raymond E.
Cabrol, Nathalie A.
Foley, Daniel J.
Franklin, Brenda J.
Geissler, Paul G.
Golombek, Matthew P.
Kuzmin, Ruslan O.
Landis, Geoffrey A.
Lemmon, Mark T.
Neakrase, Lynn D. V.
Squyres, Steven W.
Thompson, Shane D.
机构
[1] Arizona State Univ, Sch Earth & Space Explorat, Tempe, AZ 85287 USA
[2] Washington Univ, Dept Earth & Planetary Sci, St Louis, MO 63130 USA
[3] NASA, Ames Res Ctr, Moffett Field, CA 94035 USA
[4] CALTECH, Jet Prop Lab, Pasadena, CA 91109 USA
[5] US Geol Survey, Astrogeol Program, Flagstaff, AZ 86001 USA
[6] Russian Acad Sci, Vernadsky Inst, Moscow 117975, Russia
[7] NASA, Glenn Res Ctr, Cleveland, OH 44135 USA
[8] Texas A&M Univ, Dept Atmospher Sci, College Stn, TX 77843 USA
[9] Cornell Univ, Dept Astron, Ithaca, NY USA
关键词
D O I
10.1029/2006JE002743
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
[1] A full dust devil "season'' was observed from Spirit from 10 March 2005 (sol 421, first active dust devil observed) to 12 December 2005 (sol 691, last dust devil seen); this corresponds to the period L-s 173.2 degrees to 339.5 degrees, or the southern spring and summer on Mars. Thermal Emission Spectrometer data suggest a correlation between high surface temperatures and a positive thermal gradient with active dust devils in Gusev and that Spirit landed in the waning stages of a dust devil season as temperatures decreased. 533 active dust devils were observed, enabling new characterizations; they ranged in diameter from 2 to 276 m, with most in the range of 10-20 m in diameter, and occurred from about 0930 to 1630 hours local true solar time (with the maximum forming around 1300 hours) and a peak occurrence in southern late spring (L-s similar to 250 degrees). Horizontal speeds of the dust devils ranged from <1 to 21 m/s, while vertical wind speeds within the dust devils ranged from 0.2 to 8.8 m/s. These data, when combined with estimates of the dust content within the dust devils, yield dust fluxes of 3.95 x 10(-9) to 4.59(-4) kg/m(2)/s. Analysis of the dust devil frequency distribution over the inferred dust devil zone within Gusev crater yields similar to 50 active dust devils/km(2)/sol, suggesting a dust loading into the atmosphere of similar to 19 kg/km(2)/sol. This value is less than one tenth the estimates by Cantor et al. (2001) for regional dust storms on Mars.
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页数:16
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