Seasonal evolution of C 2N 2, C 3H 4, and C 4H 2 in Titan's lower stratosphere, inferred from Cassini/CIRS far-IR observations (2016)

First Author: Sylvestre Melody
Attributed to:  Solar System Planetary Science at Oxford 2016-2019 funded by STFC

Abstract

No abstract provided

Bibliographic Information

Type: Working Paper

Volume: 48

Parent Publication: AAS/Division for Planetary Sciences Meeting Abstracts #48