Tropical mountain glaciers on Mars: Altitude-dependence of ice accumulation, accumulation conditions, formation times, glacier dynamics, and implications for planetary spin-axis/orbital history
By J. Fastook, James W. Head III, David Gray Marchant, Francois Forget. 2007
143 citations recorded by the source corpus.
View Paper: https://www.semanticscholar.org/paper/2a90916093f95667e2457f5cdb3cbcc37090b62c
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
- R. Wordsworth
- Francois Forget
- Ehouarn Millour
- Jean-Baptiste Madeleine
- B. Charnay
- M. Carr
- James W. Head III
- J. Leconte
Citations in the corpus
- Geologic history of Mars (2010, result): “Glacial flow models employing the location and amount of precipitation predicted by the general circulation models produce deposits similar to those observed (Fastook et al., 2008).”
- Global modelling of the early Martian climate under a denser CO2 atmosphere: Water cycle and ice evolution (2012, background): “Geological evidence suggests that throughout much of the Amazonian, the mean annual surface temperatures of Mars have been so cold that basal melting does not occur in ice sheets or glaciers [e.g., Fastook et al., 2008, Head et al., 2010, Fastook et al., 2011].”