Chapter 1 Flashcards
Most important GHGs
CO2, CH4 & N2O
Global mean temp rise since 1850
0.4C - 14.5C
Global average sea level rise since 1850
20cm
Outline Greenhouse effect
- Solar radiation passes through atmosphere
- Most absorbed by surface, warming it & lower atmosphere
- Radiation re-emitted in all directions by GHG molecules, casing warming.
Why difficult to compare to natural forcing?
Poor data pre industrial revolution
Other GHGs contribute what amount compared to CO2?
2/3
Albedo meaning
amount of radiation the earth can reflect
How humans effected Albedo
- Heat reducing snow & ice & soot darkening
- Cities radiate more heat
- Grass reflects more than forests.
Aerosol & water vapor…
form clouds, influencing radiative balance
Nutrient cycle influenced by
nitrogen & phosphate fertilizers
Main human effects on
vegetation, albedo & carbon cycle
Natural warming effects
Volcanic eruptions, large but short lived effects.
Compounding effect of water vapor
Warmer air = more water vapor
Water vapor is a GHG
Warmer air causes further warming
Why cloud formation impacts uncertain?
keep heat in during night & winter
But, sun out in summer & daytime
Why ocean uncertainty?
Warming depends on complex patterns of currents.
Poor deep ocean data.