MAIC-2 simulation run_t14 ...

Visualization of the time-dependent H2O glaciation of Mars, simulated by MAIC-2 experiment run_t14. This is the best-fit simulation #6 by Greve et al. (2010), extended from 20 million years ago until 10 million years into the future. North up, vertical exaggeration factor ~676. Bottom panel: Obliqui...

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Bibliographic Details
Main Authors: Grieger, Björn, Greve, Ralf, Stenzel, Oliver J.
Format: Article in Journal/Newspaper
Language:English
Published: Zenodo 2011
Subjects:
Mars
Planetary ice
Obliquity
Ice cap
Polar layered deposits
Ice age
Online Access:https://dx.doi.org/10.5281/zenodo.3696125
https://zenodo.org/doi/10.5281/zenodo.3696125
Description
Summary:Visualization of the time-dependent H2O glaciation of Mars, simulated by MAIC-2 experiment run_t14. This is the best-fit simulation #6 by Greve et al. (2010), extended from 20 million years ago until 10 million years into the future. North up, vertical exaggeration factor ~676. Bottom panel: Obliquity over time. ...

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