Chapter 7: Planetary Atmospheres: Earth and Other Terrestrial Worlds Flashcards
Size of Earth’s Atmosphere
10 km thick
-consists mostly of molecular nitrogen and oxygen
pressure and density relation with altitude
pressure and density decrease with altitude because the weight of overlying layers is less
Earth’s pressure at sea level
101.325 kPa
14.7lb per sq inch
1 bar
where does the atmosphere end?
there is no clear upper boundary to where the atmosphere ends
what is considered space?
altitudes more than 100 km
- small amounts of gas are present even above 300 km
how does an atmosphere determine whether liquid water can exist on surface?
creates pressure that determines existence
how does an atmosphere create a magnetosphere
-absorbs and scatters light
-creates wind, weather, and climate
-interacts with solar wind
what is a magnetosphere
a region of space around a planet in which the planet’s magnetic field can affect charged particles
greenhouse effect
visible light passes through the atmosphere and warms a planet’s surface
earth surface temp with no greenhouse gases
well below the freezing point of water
how does the greenhouse effect trap heat?
- atmosphere absorbs infrared light from surface, trapping heat
why does burning fossil fuels increase the greenhouse effect on Earth?
burning releases carbon dioxide into the atmosphere
what determines a planet’s surface temperature?
determined by the balance between energy from sunlight it absorbs and energy of outgoing thermal radiation