<?xml version='1.0' encoding='utf-8'?>
<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:contributor>P.L. Whelley</dc:contributor>
  <dc:contributor>R. E. Arvidson</dc:contributor>
  <dc:contributor>N.A. Cabrol</dc:contributor>
  <dc:contributor>D.J. Foley</dc:contributor>
  <dc:contributor>B.J. Franklin</dc:contributor>
  <dc:contributor>P.G. Geissler</dc:contributor>
  <dc:contributor>M.P. Golombek</dc:contributor>
  <dc:contributor>R.O. Kuzmin</dc:contributor>
  <dc:contributor>G. A. Landis</dc:contributor>
  <dc:contributor>M.T. Lemmon</dc:contributor>
  <dc:contributor>L.D.V. Neakrase</dc:contributor>
  <dc:contributor>S. W. Squyres</dc:contributor>
  <dc:contributor>S.D. Thompson</dc:contributor>
  <dc:creator>R. Greeley</dc:creator>
  <dc:date>2006</dc:date>
  <dc:description>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 Ls 173.2?? to 339.5??, 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 (Ls ??? 250??). Horizontal speeds of the dust devils ranged from &lt;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 ?? 10-9 to 4.59-4 kg/m2/s. Analysis of the dust devil frequency distribution over the inferred dust devil zone within Gusev crater yields ???50 active dust devils/km2/sol, suggesting a dust loading into the atmosphere of ???19 kg/km2/sol. This value is less than one tenth the estimates by Cantor et al. (2001) for regional dust storms on Mars. Copyright 2006 by the American Geophysical Union.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1029/2006JE002743</dc:identifier>
  <dc:language>en</dc:language>
  <dc:title>Active dust devils in Gusev crater, Mars: Observations from the Mars Exploration Rover Spirit</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>