Econ II - Session 9 Flashcards
Greenhouse effect
Phenomenon within the atmosphere of the earth.
Certain gasses let short-wave light (visible light) pass but
absorb long-wave light (heat)
Earth radiation equilibrium
Incoming energy = outgoing energy (different type of radiation, longer waves)
What accelerates ice sheet melting once it started?
When the ice sheet melt, melting accelerates as lower ice faces warmer air (like up in the mountains, it’s cooler)
By what is earth’s energy balance affected?
- Increased CO2 concentration
- Increased concentration of other GHG (methane, …)
- Change in surface albedo (reflection)
- Atmospheric pollution that reflects sunlight (aerosols)
- Change in solar activity
- Carbon cycle
- three major “sinks” for CO2
Carbon cycle: how much of the emitted CO2 remains in the atmosphere (after photosynthesis, ocean absorption etc.)
- Ocean: CO2 is chemically absorbed
- Vegetation: Through photosynthesis
- Atmosphere 🫠
Negative feedback mechanism (climate)
warming –> atmosphere can hold up more water vapor –> more clouds –> cooling –> –> warming
positive feedback mechanism (climate)
warming –> ice melting –> decrease albedo –> more insolation (= Sonneneinstrahlung) absorbed –> warming
principle mechanisms of climate change
Greenhouse effect
Carbon cycle
Indicators for climate change
- Radiative forcing (GHG concentration in atmosphere)
- Temperature
- Sea level
- Ocean heat content
- Ice and snow cover
Why is the sea level rising?
- Melting mountain glaciers / greenland & arctic ice sheet –> more water
- Warmer water has more volume (thermal expansion)