Titlebook: Geology and Habitability of Terrestrial Planets; Kathryn E. Fishbaugh,Philippe Lognonné,Oleg Korabl Book 2007 Springer-Verlag New York 200

Nonconformist

思想

红润

Emergence of a Habitable Planet,cooled and condensed over ∼1,000 yrs. As it cooled the Earth degassed its volatiles into the atmosphere. It took another ∼2 Myrs for the magma ocean to freeze at the surface. The cooling rate was determined by atmospheric thermal blanketing. Tidal heating by the new Moon was a major energy source to

mitral-valve

Creating Habitable Zones, at all Scales, from Planets to Mud Micro-Habitats, on Earth and on Mars,s such as habitat linkage. The possibility of habitability first comes about during accretion, as a product of the processes of impact and volatile inventory history. To create habitability water is essential, not only for life but to aid the continual tectonic reworking and erosion that supply key

tympanometry

Water, Life, and Planetary Geodynamical Evolution,rely a substrate on which life may develop. Large-scale exchange of heat and volatile species between planetary interiors and hydrospheres/atmospheres, as well as the presence of a magnetic field, are important factors contributing to the habitability of a planet. This chapter reviews these processe

mechanism

A Comparative Study of the Influence of the Active Young Sun on the Early Atmospheres of Earth, Venupper atmospheres, and thermal and non-thermal atmospheric loss processes, the long-time evolution of planetary atmospheres and their water inventories can only be understood within the context of the evolving Sun. We compare the effect of solar induced X-ray and EUV (XUV) heating on the upper atmos

preservative

Planetary Magnetic Fields and Solar Forcing: Implications for Atmospheric Evolution,cting the habitability and chances for life to emerge on a planet. The forcing is essentially inversely proportional to the square of the distance to the Sun and, therefore, is most important for the innermost planets in our solar system—the Earth-like planets. The effect of these two forcing terms

chapel

Planetary Magnetic Dynamo Effect on Atmospheric Protection of Early Earth and Mars,osphere is protected from erosion by solar wind. The magnetic field ensures the maintenance of a dense atmosphere, necessary for liquid water to exist on the surface of Mars. We also examine the impact of the rotation of Mars on the magnetic field. When the magnetic field of Mars ceased to exist (ab

Bricklayer

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