American Geophysical Union, Geophysical Research Letters, 1(37), p. n/a-n/a, 2010
DOI: 10.1029/2009gl041426
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Near-surface perennial water ice on Mars has been previously inferred down to latitudes of about 45{\deg} and could result from either water vapor diffusion through the regolith under current conditions or previous ice ages precipitations. In this paper we show that at latitudes as low as 25{\deg} in the southern hemisphere buried water ice in the shallow (