Space weathering on airless bodies

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Space weathering on airless planetary bodies: clues from the lunar mineral hapkeite.

Physical and chemical reactions occurring as a result of the high-velocity impacts of meteorites and micrometeorites and of cosmic rays and solar-wind particles are major causes of space weathering on airless planetary bodies, such as the Moon, Mercury, and asteroids. These weathering processes are responsible for the formation of their regolith and soil. We report here the natural occurrence o...

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Sulfur Compositional Effects on Space Weathering

The reflectance spectrum of visible and near infrared light off of airless bodies in our Solar System gives us insight to surface mineralogy. However, this method of remote sensing is subjected to the space weathering effects of darkening and reddening optical spectra, along with changes to the depths of absorption bands over time. These optical changes are caused by nanophase iron blebs as a r...

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On the average temperature of airless spherical bodies and the magnitude of Earth’s atmospheric thermal effect

The presence of atmosphere can appreciably warm a planet's surface above the temperature of an airless environment. Known as a natural Greenhouse Effect (GE), this near-surface Atmospheric Thermal Enhancement (ATE) as named herein is presently entirely attributed to the absorption of up-welling long-wave radiation by greenhouse gases. Often quoted as 33 K for Earth, GE is estimated as a differe...

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ژورنال

عنوان ژورنال: Journal of Geophysical Research: Planets

سال: 2016

ISSN: 2169-9097

DOI: 10.1002/2016je005128