Environmental Physics Lecture 3 email: [email protected] web: http://people.physics.anu.edu.au/~jps107/ ChloroFlouroCarbons (CFCs) Man-made chemicals CFCl3 (Freon-11), CF2Cl2 (Freon-12) Used in aircon, refrigerators, foam, solvents, propellants Long lifetime in atmosphere CFCL3 – 45 yrs, CF2Cl2 – 100 years Can travel up to the ozone layer Takes around 15 years Chemical reactions of CFCs CFCl3 + hν (>3.5 eV, <350nm)--> CFCl2 + Cl O3 + Cl --> O2 + ClO ClO + O --> Cl + O2 ClO + O3 --> Cl + 2O2 Chlorine atom is a catalyst How will this affect ozone concentration? Ozone hole Ozone depletion Reduction in ozone corresponds to increase in stratospheric CFCs Why has it stopped? Ozone Hole Montreal Protocol instituted in 1989 Phase out production and use of ozone depleting substances contain either chlorine or bromine. If adhered to, the ozone layer is expected to recover by 2050 The greenhouse effect What is a greenhouse? What does it do? How? Absorption of light – what is the type of light we get from the sun? Greenhouses The glass or plastic in a greenhouse roof and walls is transparent to visible and infrared light. Light is absorbed by the material inside a greenhouse What materials? Light is converted to heat energy How? What happens when a photon is absorbed by a solid? Do all photons get absorbed? Absorb energy by phonon excitation – the material vibrates It then heats up. Greenhouses Heat is transferred to the gas (air) inside the greenhouse What form does this heat take? What happens to the air? If there is no roof or walls, the hot air can mix with colder air and it cools down The greenhouse traps the hot air and it stays inside The greenhouse is warmer than the surrounding environment Greenhouse effect What are we talking about? Earth’s atmosphere This is not exactly the same as how a greenhouse works! Let’s talk about blackbodies and blackbody radiation What is a blackbody? Hypothetical object, absorbs all radiation Will also radiate energy – wavelength of radiation emitted will depend on temperature Greenhouse effect Consider the Earth – it absorbs light from the Sun and warms up This is similar to a blackbody Energy from the sun is around 3.5 to 7 kWh/m2 each day However, the Earth also reflects light Reflects around 30% of sunlight. What does this mean? Greenhouse effect From consideration as a blackbody, the Earth would have an average surface temperature of around -18oC Real average surface temperature is actually 14oC – why? Atmosphere! The atmosphere traps heat that would otherwise radiate away into space What is the atmosphere made of? Nitrogen (N2) - 78 %, Oxygen (O2) - 21% , Argon (Ar) - 0.9%, Carbon dioxide (CO2) - 0.04% + others (not including water) Greenhouse effect How does the atmosphere trap heat? Does it work like the greenhouse in our previous example? No! There is no confinement of hot gas, it can freely circulate throughout the atmosphere Earth radiates photons (energy) in the wavelength range 4 – 100 µm N2, O2 and Ar DO NOT absorb radiation in these wavelengths CO2 (and H2O) DO absorb these wavelengths Greenhouse effect What happens when the infrared (IR) radiation is absorbed? Greenhouse effect So what happens to the radiation from the Earth’s surface? It is absorbed by CO2 (and other gases, H2O, methane (CH4), ozone (O3) etc…) When reemitted, some can travel back towards Earth This radiation is trapped and can then heat up the Earth further This has the effect of warming the Earth more than would be expected from just the “blackbody effect” Makes life possible… Greenhouse effect In 1850, Carbon dioxide (CO2) concentration was around 0.028 % In 1950, around 0.031 % In 2010, around 0.038 % What does an increase in CO2 mean?
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