We apply a recently proposed method to estimate heavy ion escape from Mars. The method combines in situ observations with a hybrid plasma model, which treats ions as particles and electrons as a fluid. With this method, we investigate how solar upstream conditions, including solar extreme ultraviolet (EUV) radiation, solar wind dynamic pressure, and interplanetary magnetic field (IMF) strength and cone angle, affect the heavy ion loss. The results indicate that the heavy ion escape rate is greater in high EUV conditions. The escape rate increases with increasing solar wind dynamic pressure, and decreases as the IMF strength increases. The ion escape rate is highest when the solar wind is parallel to the IMF and lowest when they are perpendi...
International audienceThe escape and precipitation of planetary ions from Mercury’s environment unde...
International audienceWe present initial Mars Atmosphere and Volatile EvolutioN (MAVEN) observations...
We present initial Mars Atmosphere and Volatile EvolutioN (MAVEN) observations and preliminary inter...
We refine a recently presented method to estimate ion escape from non-magnetized planets and apply i...
When the solar wind reaches the Mars obstacle, mass loading by planetary ions slows down the solar w...
Planetary habitability is in part determined by the atmospheric evolution of a planet; one key compo...
Escape of ions is potentially important for the evolution of volatiles on Mars, but the mechanisms a...
International audienceDuring the last decade, MAVEN space mission have emphasized a widespread spati...
Using Mars Express data from 2007 until 2020 we show how ion outflow from Mars varied over more than...
Present-day Mars is a cold and dry planet with a thin CO2-dominated atmosphere comprising only a few...
International audienceIn November 2014 the MAVEN (Mars Atmosphere and Volatile EvolutioN) spacecraft...
International audienceWe present a kinetic study to quantify the response of Mars’ atmosphere to cha...
International audienceThe escape and precipitation of planetary ions from Mercury’s environment unde...
International audienceWe present initial Mars Atmosphere and Volatile EvolutioN (MAVEN) observations...
We present initial Mars Atmosphere and Volatile EvolutioN (MAVEN) observations and preliminary inter...
We refine a recently presented method to estimate ion escape from non-magnetized planets and apply i...
When the solar wind reaches the Mars obstacle, mass loading by planetary ions slows down the solar w...
Planetary habitability is in part determined by the atmospheric evolution of a planet; one key compo...
Escape of ions is potentially important for the evolution of volatiles on Mars, but the mechanisms a...
International audienceDuring the last decade, MAVEN space mission have emphasized a widespread spati...
Using Mars Express data from 2007 until 2020 we show how ion outflow from Mars varied over more than...
Present-day Mars is a cold and dry planet with a thin CO2-dominated atmosphere comprising only a few...
International audienceIn November 2014 the MAVEN (Mars Atmosphere and Volatile EvolutioN) spacecraft...
International audienceWe present a kinetic study to quantify the response of Mars’ atmosphere to cha...
International audienceThe escape and precipitation of planetary ions from Mercury’s environment unde...
International audienceWe present initial Mars Atmosphere and Volatile EvolutioN (MAVEN) observations...
We present initial Mars Atmosphere and Volatile EvolutioN (MAVEN) observations and preliminary inter...