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The Earth’s Atmosphere

The Earth’s Atmosphere. Also water vapor (most near the surface of the earth), dust and pollutants (e.g. sulfur dioxide). A Special Note on Carbon Dioxide. present in trace amounts, but important in its effects:

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The Earth’s Atmosphere

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  1. The Earth’s Atmosphere

  2. Also water vapor (most near the surface of the earth), dust and pollutants (e.g. sulfur dioxide)

  3. A Special Note on Carbon Dioxide • present in trace amounts, but important in its effects: • a greenhouse gas (GHG) – a gas that is very effective at absorbing (trapping) and emitting radiation as heat (infrared radiation) 0.039% means 390 ppm (“ppm” = parts per million)Pre-industrial CO2 level: 275 ppmPresent CO2 level: 390 ppmSafe (?) CO2 level: 350 ppm

  4. Why is the atmosphere important? • Natural Greenhouse Effect, temperature extremes: warms Earth’s surface, reduces day/night extremes; • Ozone layer: protects against damaging ultraviolet (UV) radiation from the Sun; • Oxygen, Carbon Dioxide, Water Cycle: oxygen for humans and animals, carbon dioxide for plants, water for all (evaporation, transpiration from plants, precipitation);

  5. Atmospheric Circulation Convection cells: Warm moist air rises at equator; Cold dry air sinks at the poles; Gives rise to winds; Heat Energy and moisture: Transfers heat and moisture around the globe, to the poles;

  6. Atmospheric Layers >500 km, space station here 80-500 km, 30 °C, auroras located here 50-80 km, -75 °C, “meso” = “middle” 12-50 km, 10 °C, highest concentration of ozone 0-16 km (8 km at poles), -50 – 20 °C, most of the atmosphere’s moisture

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