

Author: Withers P. Lorenz R.D. Neumann G.A.
Publisher: Academic Press
ISSN: 0019-1035
Source: Icarus, Vol.159, Iss.1, 2002-09, pp. : 259-261
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Abstract
Each Viking Lander measured a topographic profile during entry. Comparing to MOLA, we find a vertical offset of 1–2 km in the Viking trajectory. Hence, Viking atmospheric densities and pressures at a given altitude are 10–20% too large.
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