Expert-level climatology covering climate system components, climate forcing and feedbacks, paleoclimatology, climate modeling, and climate change science.
Components: atmosphere, ocean, cryosphere, land surface, biosphere. Energy balance: incoming solar vs outgoing longwave radiation. Greenhouse effect: CO2, H2O, CH4, N2O absorb and re-emit longwave radiation. Albedo: fraction of solar radiation reflected — ice-albedo feedback amplifies warming.
Radiative forcing: change in net radiation caused by external factor (W/m2). CO2 forcing: 3.7 W/m2 per doubling of CO2 concentration. Positive feedbacks: ice-albedo, water vapor (strongest), cloud (uncertain sign). Negative feedbacks: Planck (blackbody), lapse rate. Climate sensitivity: equilibrium warming per doubling of CO2 — likely 2.5-4 C.
Ice cores: temperature (oxygen isotopes), CO2, dust, dating by annual layers. Marine sediments: foram isotopes, SST proxies, long records to millions of years. Tree rings: temperature and precipitation proxies, annual resolution. Milankovitch cycles: orbital forcing — eccentricity (100 kyr), obliquity (41 kyr), precession (23 kyr).
Energy balance models: simple, global or zonal average. GCM: general circulation models, full 3D atmosphere and ocean. CMIP: Coupled Model Intercomparison Project — ensemble of model projections. Downscaling: statistical or dynamical methods to increase spatial resolution.
| Pitfall | Fix |
|---|---|
| Confusing weather and climate | Climate is statistics of weather over 30+ years |
| Ignoring aerosol forcing | Aerosols offset some greenhouse warming |
| Single model projection as truth | Always use ensemble range for uncertainty |
| Misinterpreting paleo proxies | Proxies integrate multiple climate variables |