4.4 - Atmosphere Flashcards
1
Q
Gases of the Earth’s atmosphere
A
- 78% - Nitrogen: Mostly in the form of N2 (unuseable to plants without being fixed)
- 21% - Oxygen: Produced by photosynthesis in plants & needed for human/animal respiration
- 0-4% - Water Vapor: Varies by region & conditions; acts as a temporary GHG, but less concerning than CO2 (Quickly cycles through atmosphere)
- .93% - Argon: Inert, noble gas
- .04% - CO2: Most important GHG; leads to global warming. Removed from atmosphere by photosynthesis
2
Q
Layers and characteristics of the earth’s atmosphere (kinda long…)
A
- troposphere
- tropo = change (weather occurs here)
- 0-16km
- most dense due to pressure of other layers above it
- Most of the atmosphere’s gas molecules are found here
- Ozone (O3) in the troposphere is harmful to humans (respiratory irritant) and damages plant
stomata, and forms smog - Stratosphere
- “S” for second
- 16-60km
- less dense due to less pressure from layers above
- Thickes O3 layer is found here; absorbs UV-B and UV-C rays, which can mutate the DNA of
animals (cancer) - Mesosphere
- Meso = Middle
- 60-80km
- even less dense - Thermosphere
- Therm = hottest temp
- absorbs harmful X-rays and UV radiation
- charged gas molecules glow under intense solar radiation producing northern lights - Exosphere
- outermost layer where atmosphere merges with space
3
Q
Temperature gradient of the earth’s atmospheric layers
A
- Troposphere - temperature decreases as the air gets further from the warmth of the earth’s surface
- Stratosphere - temperature increases because the top layer of the stratosphere is warmed by UV rays (like a pool’s surface)
- Mesosphere - temperature decreases because density decreases, leaving fewer molecules to absorb sun (coldest place on earth -150°F)
- Thermosphere - temperature increases due to absorption of highly energetic solar radiation (the hottest place on earth: 3,100°F)
- Exosphere - no temperature because it merges with space
4
Q
Temperature gradient
A
layers of earth’s atmosphere are based on where temperature gradients change with distance form earth’s surface