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Polar warming in the middle atmosphere of Mars

✍ Scribed by Drake Deming; Michael J. Mumma; Fred Espenak; Theodor Kostiuk; David Zipoy

Publisher
Elsevier Science
Year
1986
Tongue
English
Weight
1002 KB
Volume
66
Category
Article
ISSN
0019-1035

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The atmospheric structure of Triton in the altitude range 25-150 km shows an unexpectedly steep thermal gradient of 0.26 K km -1 above 50 km altitude, with a nearly isothermal profile below. The upper part of the profile can be explained by downward conduction of heat deposited by magnetospheric ele