L8 - Climate Forcing Extended Flashcards
What happens when there’s fewer low hanging clouds (over ocean vs land)?
Ocean: Fewer low-hanging clouds result in greater long-term energy absorption because of the ocean’s thermal inertia, which allows it to store heat over extended periods. This contributes to large-scale climate changes.
Land: The effects are more immediate, with stronger local heating and faster temperature changes, leading to potential impacts on ecosystems, agriculture, and human infrastructure.
- can amplify global warming as less albedo effect
- influences weather
explain lapse rate feedback
- Initially reduced LW emissions at tropopause when increased GHG
- Restored balance at tropopause after some time
- BUT increased LW radiation at surface
are gases well mixed in the stratosphere?
No due to the temperature profile
Describe polar amplification?
Increased heating at the poles due to albedo effect and increase in lapse rate, where there is a stronger temp change at the surface than in the tropopause
Greenhouse effect components?
Emissivity AND temperature difference between surface and atmosphere (lapse rate)
What is effective temperature?
Combination of Ta of upper and lower atmosphere (cooler at top) - determines how much goes through tropopause to troposphere
What is the Global Carbon Project?
The GCP integrates knowledge of GHG for human activities and the earth system. Includes budgets for 3 dominant GHG and efforts in urban, regional, cumulative and negative emissions
Budget
total amount of emissions that can be released while staying within climate change target e.g. limiting warming to 2 degrees
Budget imbalance
difference between estimated emissions and sinks. It is total emissions minus the estimated growth in the atmosphere, land and ocean sinks. Reflects the limits of our understanding of the carbon cycle
Bunkers
fossil fuels used for international shipping and aviation
Largest contributors to land use change fluxes?
Brazil, Indonesia and DR Congo
What is the substitution method?
When non-fossil sources are scaled up by an assumed fossil efficiency of 0.38