2 6-2003
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The document discusses several topics related to the greenhouse effect and global warming: 1. Greenhouse gases like carbon dioxide and methane absorb infrared radiation, trapping heat in the lower atmosphere and causing the greenhouse effect. 2. An increase in greenhouse gases leads to an enhanced greenhouse effect and global warming as the Earth's surface temperature rises. 3. While climate varies naturally, determining if changes in things like precipitation and temperature are due to natural variability or climate change caused by human activity is challenging for scientists.
2 6-2003
- 1. Last Class How does variability in the earth’s physical structure affect the transformations of energy? - albedo of different “spheres”; clouds What is the physical structure of the atmosphere? - multi-layered, with little chemical interaction - most of the mass is near the surface What is the chemical structure of the atmosphere? - nitrogen by far the most common element - oxygen is second most common - greenhouse gasses are small in amount, but important!
- 3. Structure of the Atmosphere Thermosphere Mesosphere Ozone Maximum Stratosphere Troposphere Temperature
- 4. How does energy input to the earth surface vary across the globe? http://www.ems.psu.edu/Courses/earth002/0402G_M.htm
- 5. This Class - The Green House Effect and Global Warming How is energy distributed to the earth’s surface? What are greenhouse gases and the greenhouse effect? Impact of an increase in atmospheric CO2 on greenhouse effect Recent changes in greenhouse gas concentrations Relationship between the greenhouse effect and global warming
- 6. The “Greenhouse Effect” The Earth’s surface thus receives energy from two sources: the sun & the atmosphere – As a result the Earth’s surface is ~33°C warmer than it would be without an atmosphere Greenhouse gases are transparent to shortwave but absorb longwave radiation – Thus the atmosphere stores energy
- 7. Electromagnetic Spectrum incoming outgoing
- 8. 1. Shorter, high Energy wavelengths Hit the earths Surface 2. Incoming energy Is converted to heat
- 9. 3. Longer, infrared Wavelengths hit Greenhouse gas Molecules in the atmosphere 4. Greenhouse gas Molecules in the Atmosphere emit Infrared radiation Back towards earth
- 10. 78% nitrogen 20.6% oxygen < 1% argon 0.4% water vapor 0.036% carbon dioxide traces gases: Ne, He, Kr, H, O3 Methane, Nitrous Oxide
- 11. Absorption Spectra of Atmospheric Gases Visible UV Infrared CH4 N2O O2 & O3 CO2 H2O atmosphere WAVELENGTH (micrometers) Anthes, p. 55
- 14. Selected Greenhouse Gases • Carbon Dioxide (CO2) – Source: Fossil fuel burning, deforestation Anthropogenic increase: 30% Average atmospheric residence time: 500 years Methane (CH4) – Source: Rice cultivation, cattle & sheep ranching, decay from landfills, mining Anthropogenic increase: 145% Average atmospheric residence time: 7-10 years Nitrous oxide (N2O) – Source: Industry and agriculture (fertilizers) Anthropogenic increase: 15% Average atmospheric residence time: 140-190 years
- 15. Summary Greenhouse gases absorb infrared radiation and prevent it from escaping to space. Carbon dioxide, methane, and nitrous oxide are very good at capturing energy at wavelengths that other compounds miss
- 16. Greenhouse Effect & Global Warming • The “greenhouse effect” & global warming are not the same thing. – Global warming refers to a rise in the temperature of the surface of the earth • An increase in the concentration of greenhouse gases leads to an increase in the the magnitude of the greenhouse effect. (Called enhanced greenhouse effect) – This results in global warming
- 17. Climate Change vs. Variability 14.5 58.0 14.4 57.8 14.3 Variability 57.6 14.2 14.1 Average 57.4 14.0 57.2 13.9 57.0 13.8 56.8 13.7 56.6 13.6 56.4 13.5 56.2 13.4 1840 1860 1880 1900 1920 1920 1940 1960 1980 2000 www.gcrio.org/ipcc/qa/cover.html (modified)
- 18. Climate Change vs. Variability Climate variability is natural. Even in a stable climate regime, there will always be some variation (wet/dry years, warm/cold years) A year with completely “average” or “normal” climate conditions is rare The challenge for scientists is to determine whether any increase/decrease in precipitation, temperature, frequency of storms, sea level, etc. is due to climate variability or climate change.
- 20. Radiation is not evenly distributed over the Surface of the earth. The northern latitudes have an energy deficit and the low latitude/ equator has an excess. But the low latitudes don’t indefinitely get hotter and the northern latitudes don’t get colder. Why? The atmosphere and ocean transfer energy from low latitudes to high
- 21. Atmospheric Pressure Decreases With Height Above 99% Most of the energy is captured close to the Above 90% surface That energy Above 50% drives climate and weather Pressure (mb) 50 percent of mass of the atmosphere is within 6 km of the surface
- 22. Atmospheric Feedbacks POSITIVE NEGATIVE Increased CO2 More water vapor & other + changes Higher temperature + Increased cloud cover More water vapor More reflected solar radiation – More absorbed infrared radiation Lower temperature + + Higher temperature Less water vapor + More water vapor