ozone hole

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Ozone Hole • 1985, British scientists reported a sudden large depletion in the Ozone over the south pole • Simultaneous satellite measurements confirmed the decrease, but were rejected by the processing software- the decrease seen was so large it was rejected by the data quality control algorithms. • When the data were re-run through the processing programs without the data quality flags, the ozone hole had been seen all the way back to 1976!

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Ozone Hole. 1985, British scientists reported a sudden large depletion in the Ozone over the south pole Simultaneous satellite measurements confirmed the decrease, but were rejected by the processing software-the decrease seen was so large it was rejected by the data quality control algorithms. - PowerPoint PPT Presentation

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Page 1: Ozone Hole

Ozone Hole• 1985, British scientists reported a sudden large

depletion in the Ozone over the south pole• Simultaneous satellite measurements confirmed

the decrease, but were rejected by the processing software-the decrease seen was so large it was rejected by the data quality control algorithms.

• When the data were re-run through the processing programs without the data quality flags, the ozone hole had been seen all the way back to 1976!

Page 2: Ozone Hole

Causes• Unique set of conditions in the

atmosphere at the south pole.• Polar Stratospheric Clouds (PSC)

are clouds in the winter polar stratosphere at altitudes of 15,000–25,000 meters (50,000–80,000 ft).

• Due to their high altitude and the curvature of the surface of the Earth, these clouds will receive sunlight from below the horizon and reflect it to the ground, shining brightly well before dawn or after dusk.

• PSCs form at very low temperatures, below −78 °C.

Page 3: Ozone Hole

PSCs and Ozone

• Ordinarily, most of the chlorine in the stratosphere resides in stable "reservoir" compounds, primarily hydrochloric acid (HCl) and chlorine nitrate (ClONO2).

• During the Antarctic winter and spring, reactions on the surface of the polar stratospheric cloud particles convert these "reservoir" compounds into reactive free radicals (Cl and ClO).

• The clouds can also remove NO2 from the atmosphere by converting it to nitric acid, which prevents the newly formed ClO from being converted back into ClONO

Page 4: Ozone Hole

What is being done• 1976 Report by the National Academy of Science that there was credible

scientific evidence for ozone depletion– US and several other countries banned the use of CFC in aerosol spray cans

• 1985 Vienna Convention for the Protection of the Ozone Layer signed– Established a framework for the negotiation of international agreements

regulating ozone depleting substances• 1987 Montreal Protocol is signed by 43 nations

– Froze CFC production at 1986 levels and reduce it to 50% by 1999– Follow up meeting in London modified it to to phase out CFCs entirely by 2000– This date was moved up to 1996 in 1992

• CFCs replaced now by HCFCs or HFC (which are greenhouse gases)– Most commonly used in the US is HFC-134a (R-134a) which has replaced CFCs

in automobile air conditioners

Page 5: Ozone Hole

Effect of these initiatives• Atmospheric concentrations have been declining• Antarctic Ozone hole will continue for decades• Expected to see Ozone concentrations increase

by 5-10% in the lower stratosphere by 2020• A return to pre 1980 levels is expected by 2060-

2075.• Eventual complete recovery of the ozone will

occur• Delays will be the result of developing countries

which employ CFCs

Page 6: Ozone Hole

Global Warming• The name given to the increase in the

average temperature of the Earth’s near surface temperature and oceans that has occurred since the middle of the 20th century.

• In the graph to the right, panel a gives the Earth's surface temperature is shown year by year (red bars) and approximately decade by decade (black line, panel b gives the year by year (blue curve) and 50 year average (black curve) variations of the average surface temperature of the Northern Hemisphere for the past 1000 years have been reconstructed from "proxy" data calibrated against thermometer data.

Page 7: Ozone Hole

Greenhouse effect• Main culprit behind global

warming• Sunlight enters the atmosphere

and warms the Earth (UV, visible, IR)

• At night, Earth radiates heat energy it gained during the day(mostly at IR wavelengths)

• Not all of this energy escapes the atmosphere-some of it is absorbed and re-emitted back into the atmosphere, warming the atmosphere and the Earth.

• Not necessarily a bad thing-without it the Earth would be cold and life (a least as we know it) would not be possible

Page 8: Ozone Hole

Venus• Hottest planet in the solar

system• But not the closest to the sun• Atmosphere is 96.5% carbon

dioxide• Venus once had immense

amounts of water, but no ozone layer-the UV radiation broke up the water molecules

• Unfortunate, water absorbs carbon dioxide wand mitigates the greenhouse effect

• Resulted in an extreme greenhouse effect

Page 9: Ozone Hole

Greenhouse effect-What could happen

• Global temperatures rise until boiling point of water is reached

• As water boils away, it becomes water vapor in the atmosphere, accelerating the heat rise (called positive feedback).

• At a few hundred degrees celsius, carbon dioxide would be released from the rocks (sublimation), accelerating the heating again

• Eventually the Earth would stabilize at surface temperatures similar to Venus (T=860F)

• Worst case, not realistic scenario

Page 10: Ozone Hole

Greenhouse Gasses –in order of importance

• water vapor• carbon dioxide• methane• nitrous oxide• ozone• CFCs

Page 11: Ozone Hole

Changes in greenhouse gas concentrations

• Historical variations can be tracked via analysis of ice cores– Ice core - a core sample (a cylindrical section of a naturally occurring

medium consistent enough to hold a layered structure) from the accumulation of snow and ice over many years that have re-crystallized and have trapped air bubbles from previous time periods.

– The composition of these ice cores provides a picture of the climate at the time.

– Record for over 800,000 years

Gas Preindustrial Level Current Level Increase since 1750 Carbon dioxide 280 ppm 387ppm 104 ppm Methane 700 ppb 1,745 ppb 1,045 ppb Nitrous oxide 270 ppb 314 ppb 44 ppb CFC-12 0 533 ppt 533 ppt

Page 12: Ozone Hole

What do the ice cores tell us?

• Natural variations occur in the greenhouse gas concentrations

Page 13: Ozone Hole

Post industrial revolution

Page 14: Ozone Hole

Man made sources of greenhouse gasses

• Also called Anthropogenic, which designates an effect or object resulting from human activity

• burning of fossil fuels and deforestation leading to higher carbon dioxide concentrations. – Account for one third of total anthropogenic CO2 emissions.

• livestock enteric fermentation and manure management, paddy rice farming, land use and wetland changes, pipeline losses, and covered vented landfill emissions leading to higher methane atmospheric concentrations. Many of the newer style fully vented septic systems that enhance and target the fermentation process also are sources of atmospheric methane.

• use of chlorofluorocarbons (CFCs) in refrigeration systems, and use of CFCs and halons in fire suppression systems and manufacturing processes.

• agricultural activities, including the use of fertilizers, that lead to higher nitrous oxide (N2O) concentrations.

Page 15: Ozone Hole

What are we seeing?• Since 1860-1900, global

surface temperatures have increased by 1.35 F

• Urban heat island effect only accounts for 0.02 C rise

• Since 1979 land T have increased twice as fast as ocean temperatures

• Temperatures on the lower troposphere have have increased by 0.62 between 1979 and 2000.

Page 16: Ozone Hole

Hold on, could it be the sun?

• No overall increase in solar brightness in over 1000 years

• Solar cycles do cause small variations in brightness, but not enough to account for what has been seen

• No its not the sun

Page 17: Ozone Hole

Feedback-making the problem worse (or better)

• Positive feedback-when the warming induces further warming

• Negative feedback – when the warming induces a cooling