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
β¦ LIBER β¦
Thin stratified structure of the middle atmosphere
β Scribed by G.M. Grechko; A.S. Gurvich
- Book ID
- 107936672
- Publisher
- Elsevier Science
- Year
- 1990
- Tongue
- English
- Weight
- 433 KB
- Volume
- 10
- Category
- Article
- ISSN
- 0273-1177
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