Skip to main content

Official Journal of the Asia Oceania Geosciences Society (AOGS)

Figure 6 | Geoscience Letters

Figure 6

From: Current understanding of the aeronomy of Mars

Figure 6

Viking plasma temperatures. Temperature profiles measured by the two Vikings [5,16] were nearly identical. On the Viking 1 entry (right), the ion temperature increased from the low altitude neutral temperature Tn (deduced from the neutral scale height) to the measured thermal electron temperature Te1at high altitudes. The electron temperatures Te2 and Te3 are inferred estimates of the presence of photoelectrons and a hotter population from the magnetosheath. Tr and Tc are theoretical models of the electron temperature from [4] and [17].

Back to article page