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Understanding the Greenhouse Effect:

Understanding the Greenhouse Effect:. Synposis : Students plot diurnal temperature observations to compare the relative magnitude of the greenhouse effect under clear and cloudy-sky conditions. Understanding the Greenhouse Effect:. Learning Objectives :

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Understanding the Greenhouse Effect:

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  1. Understanding the Greenhouse Effect: • Synposis:Students plot diurnal temperature observations to compare the relative magnitude of the greenhouse effect under clear and cloudy-sky conditions

  2. Understanding the Greenhouse Effect: • Learning Objectives: • 1) Relate strength of the greenhouse effect to common experience • 2) Apply physical principles to characterize response to increased greenhouse gases • 3) Critically evaluate human-caused vs solar-caused hypotheses for recent warming.

  3. The Greenhouse Effect:Fundamental Questions & Context • What is the Greenhouse Effect? • How big is the effect? • Why are cloudy nights warmer than clear nights?

  4. Electromagnetic (EM) radiation, radiation processes • “Clear Sky” Exercise • Earth-Sun System • Greenhouse Gases • “Cloudy Sky” Exercise The Greenhouse Effect

  5. Background Information • Electromagnetic (EM) radiation • Solar and Terrestrial Emission • Radiation Processes and Interactions • Water Vapor is a Greenhouse Gas (selective absorpotion)

  6. Central Project Question Knowing that water vapor is a potent greenhouse gas, what do you expect is the short-term effect of cloud cover on your local temperature?

  7. Electromagnetic (EM) radiation, radiation processes • “Clear Sky” Exercise • Earth-Sun System • Greenhouse Gases • “Cloudy Sky” Exercise • Earth vs Moon The Greenhouse Effect

  8. Clear Sky Anticipation Questions For a weather station located at Des Moines, Iowa , consider the following questions regarding the diurnal cycle during both winter (January) and summer (July). • Why does temperature change through the day? 2) Assuming a cloudless day, plot your expectations for the diurnal cycle of temperature using the blank template figure.

  9. Hour of Day Hour of Day

  10. Anticipation Questions (continued…) Diurnal cycle during both winter (January) and summer (July) at Des Moines Iowa. 3) Indicate the time of sunrise and sunset in your figure. 4) What, specifically, causes temperature to increase or decrease? 5) How do summer and winter differ? Why?

  11. Hour of Day Hour of Day

  12. Anticipation Questions (summary) • Diurnal cycle during both winter (January) and summer • (July) at Des Moines Iowa. • Indicate the time of sunrise and sunset in your figure. • What, specifically, causes temperature to increase or decrease? • How do summer and winter differ? Why?

  13. Realization Data Source:Airport at Des Moines, IA from 1945-2004 (NCDC Surface Airways) Observation Variables:Temperature and cloud ceiling height (the height of the lowest cloud layer, if present) • Methodology: • Sort data and select only “clear sky” conditions • Compute the average diurnal cycle • Repeat for both January and July data

  14. Hour of Day Hour of Day

  15. Clear Sky Contemplation • Why does temperature change through the day? • How does temperature decrease? • How do summer and winter differ?

  16. Electromagnetic (EM) radiation, radiation processes • “Clear Sky” Exercise • Earth-Sun System • Greenhouse Gases • “Cloudy Sky” Exercise • Earth vs Moon The Greenhouse Effect

  17. Radiation: Fundamental Principles • All objects emit EM radiation; the wavelength and energy emitted depends on the object’s temperature • As Temperature increases, • total emission increases • As Temperature increases, • wavelength of peak emission decreases

  18. Solar and Terrestrial Radiation UV | Visible | IR NOTE: Log Scale! Sun Earth

  19. (No Atmosphere Case) = Earth, Absorbed = Emitted

  20. Solar Radiation Terrestrial Radiation “Radiative Equilibrium” Incoming = Outgoing Stable Temperature

  21. Electromagnetic (EM) radiation, radiation processes • “Clear Sky” Exercise • Earth-Sun System • Greenhouse Gases • “Cloudy Sky” Exercise • Earth vs Moon The Greenhouse Effect

  22. Selective Absorption in the Atmosphere

  23. …“transparent” for sunlight • …only partially transparent to Infrared Radiation (…from Earth’s Surface) • … “warmed” via radiation (However, sensible heat and convection also “warm” the atmosphere) Greenhouse Gases are…

  24. Electromagnetic (EM) radiation, radiation processes • “Clear Sky” Exercise • Earth-Sun System • Greenhouse Gases • “Cloudy Sky” Exercise • Earth vs Moon The Greenhouse Effect

  25. Cloudy Sky Anticipation Questions Diurnal cycle during both winter (January) and summer (July) at Des Moines Iowa. 1) How might temperature differ between clear and cloudy sky conditions? 2) Draw your expectations on the figure provided, labeling the clear and cloudy sky lines.

  26. Hour of Day Hour of Day

  27. Hour of Day Hour of Day

  28. Cloudy Sky Contemplation • Why is the cloudy sky temperature relatively flat? • How does clear sky temperature get both hotterand colder than the cloudy sky temperature?

  29. Incoming Solar Earth’s Surface Emits Infrared Radiation Greenhouse Process

  30. Greenhouse Process • Greenhouse Gases • Absorb IR

  31. Greenhouse Process • Greenhouse Gases • Absorb IR • Emit IR

  32. Greenhouse Process NET EFFECT: Earth’s surface Warmed by TWO Heating sources

  33. Greenhouse Process What if we add more Greenhouse Gases?? TWO Heating sources

  34. Summary • GHGs absorb IR emitted by Earth’s Surface • The gases also emit IR back to the surface, providing an additional heating source. • An example of this effect is the relative warmth of cloudy nights. • Additional GHGs will increase surface temperature in the same way as enhanced cloud cover. The Greenhouse Effect

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