학술논문
Secular Climate Change on Mars: An Update Using MSL Pressure Data
Document Type
Report
Author
Haberle, R. M; Gomez-Elvira, J; Juarez, M. de la Torre; Harri, A.-M; Hollingsworth, J. L; Kahanpaa, H; Kahre, M. A; Lemmon, M; Martin-Torres, F. J; Mischna, M; Moores, J. E; Newman, C; Rafkin, S. C. R; Renno, N; Richardson, M. I; Rodriguez-Manfredi, J. A; Thomas, P; Vasavada, A. R; Wong, M. H; Zorzano-Mier, M.-P
Source
Subject
Language
English
Abstract
The South Polar Residual Cap (SPRC) on Mars is an icy reservoir of CO2. If all the CO2 trapped in the SPRC were released to the atmosphere the mean annual global surface pressure would rise by approx. 20 Pa. Repeated MOC and HiRISE imaging of scarp retreat rates within the SPRC have led to the suggestion that the SPRC is losing mass. Estimates for the loss rate vary between 0.5 Pa per Mars Deacde to 13 Pa per Mars Decade. Assuming 80% of this loss goes directly to the atmosphere, and that the loss is monotonic, the global annual mean surface pressure should have increased between approx. 1-20 Pa since the Viking mission (19 Mars years ago).