Chapter 8- Atmospheres of Terrestial Planets Flashcards
Primary atmospheres
H, He parts of original solar nebula. Some captured by inner planets before nebular gases dispersed by eruptions of growing protosun. But these light gases were soon lost.
Escape speed
Minimum speed for gas molecule to become unbound from planet
Distribution of molecular speeds
Temperature determines distribution of molecular speeds for molecules in atmosphere. Lighter molecules have higher speeds for same temperature than do heavier molecules. If a significant fraction of molecules have speeds near the escape speed, atmosphere will escape.
Jupiter: massive (high escape speed) and cold (low molecular speeds) has retained its atmosphere.
Moon: low mass (low escape speed) has lost its atmosphere.
Mercury: low mass, high temp – almost no atmosphere.
Secondary atmospheres
Volcanism supplies gases trapped in interior materials(water vapor, carbon dioxide, sulfur dioxide, nitrogen).
Impacts from comets might bring in water vapor, carbon monoxide, methane, ammonia (decomposed by sunlight into hydrogen [escapes], nitrogen)
Greenhouse effect
Solar radiation passes through atmosphere and strikes Earth,re-radiated as infrared. IR is absorbed by greenhouse gasses (CO2, H20) and changed to heat.