An analysis of the collisional transition between the lower atmosphere and the collisionless exosphere is carried out based upon an integral formulation of the Boltzmann equation. This investigation utilizes a collision model which is a combination of Lorentz-gas and relaxation collision models. The results of this analysis indicate that intermolecular collisions act in two ways to affect the atmosphere. First, there is a critical layer, similar to the apparent photospheric surface of the Sun, from which the material escaping from the planet originates. This layer is determined by collision suffered by particles moving on orbits which skim tangentially by the planet. Secondly, collisions reduce the vertical flux of material in a manner anal...
We discuss coupled ionosphere/thermosphere models of Mars and implications for the photochemical esc...
A simple, idealized model for the rapid escape of a hydrogen thermosphere provides some quantitative...
Collisionless Boltzmann equation for model of rotating and nonuniform planetary exosphere
This work aims to provide an accurate description and calculations of collision frequencies in condi...
The present state of planetary exospheres is determined largely by satellite and ground based obser...
A brief selection of problems occurring in the interpretation of planetary atmospheres, the resoluti...
The equations of gas dynamics are extensively used to describe atmospheric loss from solar system bo...
International audienceIn the recent years, the presence of dications in the atmospheres of Mars, Ven...
With a Monte Carlo model we investigate the escape of hot oxygen and carbon from the Martian atmosph...
The impact of a large extraterrestrial body onto a planet deposits considerable energy in the atmosp...
Aims. In this Letter, we calculate for the first time the full transonic hydrodynamic escape of an E...
NASA has undertaken a concerted effort to generate a complete model for the chemical reactions and o...
We examine the mechanisms by which the atmosphere can be eroded by giant impacts onto Earth-like pla...
The history of the martian atmosphere and climate over time cannot be properly understood without kn...
Abstract: The problem of solid body vaporization into vacuum is considered. Evolution of ...
We discuss coupled ionosphere/thermosphere models of Mars and implications for the photochemical esc...
A simple, idealized model for the rapid escape of a hydrogen thermosphere provides some quantitative...
Collisionless Boltzmann equation for model of rotating and nonuniform planetary exosphere
This work aims to provide an accurate description and calculations of collision frequencies in condi...
The present state of planetary exospheres is determined largely by satellite and ground based obser...
A brief selection of problems occurring in the interpretation of planetary atmospheres, the resoluti...
The equations of gas dynamics are extensively used to describe atmospheric loss from solar system bo...
International audienceIn the recent years, the presence of dications in the atmospheres of Mars, Ven...
With a Monte Carlo model we investigate the escape of hot oxygen and carbon from the Martian atmosph...
The impact of a large extraterrestrial body onto a planet deposits considerable energy in the atmosp...
Aims. In this Letter, we calculate for the first time the full transonic hydrodynamic escape of an E...
NASA has undertaken a concerted effort to generate a complete model for the chemical reactions and o...
We examine the mechanisms by which the atmosphere can be eroded by giant impacts onto Earth-like pla...
The history of the martian atmosphere and climate over time cannot be properly understood without kn...
Abstract: The problem of solid body vaporization into vacuum is considered. Evolution of ...
We discuss coupled ionosphere/thermosphere models of Mars and implications for the photochemical esc...
A simple, idealized model for the rapid escape of a hydrogen thermosphere provides some quantitative...
Collisionless Boltzmann equation for model of rotating and nonuniform planetary exosphere