AEROSOLS, CLOUDS AND CLIMATE Flashcards
Climate - definition
Long-term average of atmospheric elements. Driven by a balance in energy.
Things affecting radiation on earth
earth surface: heating by absorption, cooling by reflection (albedo).
Atmosphere: Absorption by clouds and greenhouse gases and reflection by clouds and aerosols
Gases that absorb short wave/long wave radiation
Short wave: O2 AND O3. Long wave: • H2O, CO2, CH4, N2O, O3 AND CFC
Albedo percent
about 28 %
Improvements needed for the climate model to be a good forecast
- MORE LAYERS ARE NEEDED
* SPATIAL AND TEMPORAL RESOLUTION MUST BE ADDED
The scattering of light by aerosols depend on
size of particle. Strongest scattering when Particle diameter>radiation wavelength
Effect of relative humidity on scattering
Water vapour is a poor scatterer of radiation so hygroscopic growth of particles at high humidity causes increased scattering.
Sulfate
created by human emissions of SO2. Important component of aerosols. Negative RF
Effects of black carbon
Fresh BC absorbs light and heats atmosphere. Aged black carbon reflects more. Could decrease albedo if it lands on snow. Possive RF
Radiative forcing
Incoming radiation-outgoing radiation
RF>0 warms climate. RF<0 cools climate
Climate effect of clouds
RF negative as a whole. Negative because they increase albedo. Positive because they absorb long wave radiation.
Clouds with cooling effect
Lower and middle clouds such as cumulus, nimbostratus, stratocumulus, stratus and altostratus.
Clouds with heating effect
High clouds such as cirrus, cirrustratus, cirrucumulus and cumulonimbus
RCP
Representative concentration pathway
RCP 2.6 vs RCP 8.5
- 6: global efforts to reduce emissions
8. 5: business as usual