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Last Class How does variability in the earth’s physical structure affect

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

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Last Class How does variability in the earth’s physical structure affect

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  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!

  2. Structure of the Atmosphere Thermosphere Mesosphere Ozone Maximum Stratosphere Troposphere Temperature

  3. How does energy input to the earth surface vary across the globe? http://www.ems.psu.edu/Courses/earth002/0402G_M.htm

  4. 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

  5. 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

  6. Electromagnetic Spectrum incoming outgoing

  7. 1. Shorter, high Energy wavelengths Hit the earths Surface 2. Incoming energy Is converted to heat

  8. 3. Longer, infrared Wavelengths hit Greenhouse gas Molecules in the atmosphere 4. Greenhouse gas Molecules in the Atmosphere emit Infrared radiation Back towards earth

  9. 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

  10. Absorption Spectra of Atmospheric Gases Visible Infrared UV CH4 N2O O2 & O3 CO2 H2O atmosphere WAVELENGTH (micrometers) Anthes, p. 55

  11. 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

  12. 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

  13. 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 themagnitude of the greenhouse effect. (Called enhanced greenhouse effect) • This results in global warming

  14. 14.5 58.0 14.4 57.8 14.3 Variability 57.6 14.2 Average 57.4 14.1 57.2 14.0 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) Climate Change vs. Variability

  15. 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.

  16. Global Energy Redistribution

  17. 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

  18. Above 99% Above 90% Above 50% Pressure (mb) Atmospheric Pressure Decreases With HeightMost of the energy is captured close to the surfaceThat energy drives climate and weather 50 percent of mass of the atmosphere is within 6 km of the surface

  19. Atmospheric Feedbacks NEGATIVE POSITIVE More water vapor & other changes Increased CO2 + Higher temperature Increased cloud cover + More water vapor More reflected solar radiation – More absorbed infrared radiation Lower temperature + + Less water vapor Higher temperature + More water vapor

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