UV causes a chlorine atom to break away from the CFC molecule
The free chlorine atom hits an ozone molecule
The chlorine atom pulls one oxygen atom away.
A free oxygen atom hits the chlorine monoxide molecule
The result is another free chlorine atom
Free chlorine will continue to deplete ozone in the stratosphere
Incoming solar radiation: UV and visible light
1/3rd reflected back into space
The remaining light is absorbed by clouds and the planet’s surface
This radiation is either absorbed by the GHGs or emitted into space
More GHGs = more IR absorbed & emitted back to earth
This process should be in equilibrium; short term, inputs might be higher or lower, which causes global warming/cooling (ice ages)
H2O Vapor: Absorbs more IR than anything else, but does not persist
CO2
CH4 (methane)
H2O (nitrous oxide)
O3 (ozone)
CFCs (not natural)
Volcanoes: ash reflects incoming radiation, so a cooling effect
Decomposition & Digestion: Dead organic matter is converted into CO2 unless there is not enough O2. If there is not enough O2, it’s converted to CH4 (methane)
Denitrification: How we get N2O or nitrogen cycle
Evaporation and Evapotranspiration: water vapor
Thermal expansion of ocean water
Disease vectors spreading from the tropics to the poles
Rising sea levels
Population movements
Global climate change
Population dynamics
Excess GHGs in the atmosphere
Melting ice sheets
Polar ice melting
Glaciers melting
Permafrost melting
Ocean acidification: CO2 dissolves in water to form H2CO3 (carbonic acid). Dissolves shells/skeletons of marine organisms (crustaceans, mollusks, coral)
Sea level Rise
Criminalizing poaching
Protecting animal habitats
Biosphere reserves: contain zones that vary in the allowed amount of impact. The central core, buffer zone, transition area
Legislation
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