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National Aeronautics and Space Administration The Greenhouse Effect www.nasa.gov Dr. Lin H. Chambers, NASA Langley Research Center Hampton, Virginia NASA Climate Day Workshop, Oct. 2011
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The Greenhouse Effect

Feb 23, 2016

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National Aeronautics and Space Administration. The Greenhouse Effect. Dr. Lin H. Chambers, NASA Langley Research Center Hampton, Virginia NASA Climate Day Workshop , Oct. 2011. www.nasa.gov . The Electromagnetic Spectrum. http://mynasadata.larc.nasa.gov/ElectroMag.html. - PowerPoint PPT Presentation
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Page 1: The Greenhouse Effect

National Aeronautics and Space Administration

The Greenhouse Effect

www.nasa.gov

Dr. Lin H. Chambers, NASA Langley Research Center

Hampton, Virginia

NASA Climate Day Workshop, Oct. 2011

Page 2: The Greenhouse Effect

National Aeronautics and Space Administration 2

The Electromagnetic Spectrum

http://mynasadata.larc.nasa.gov/ElectroMag.html

Page 3: The Greenhouse Effect

National Aeronautics and Space Administration 3

The Blackbody Spectrum – The Sun

http://phet.colorado.edu/simulations/sims.php?sim=Blackbody_Spectrum

Page 4: The Greenhouse Effect

National Aeronautics and Space Administration 4

The Blackbody Spectrum – Light Bulb

http://phet.colorado.edu/simulations/sims.php?sim=Blackbody_Spectrum

Page 5: The Greenhouse Effect

National Aeronautics and Space Administration 5

The Blackbody Spectrum – Light Bulb

http://phet.colorado.edu/simulations/sims.php?sim=Blackbody_Spectrum

Note Scale Change!

Page 6: The Greenhouse Effect

National Aeronautics and Space Administration 6

The Electromagnetic Spectrum

http://radiojove.gsfc.nasa.gov/education/educ/radio/tran-rec/exerc/iono.htm

Peak of Earth emission ~10 mm = 104 nm

Page 7: The Greenhouse Effect

National Aeronautics and Space Administration 7

The Earth’s Energy Budget

http://mynasadata.larc.nasa.gov/preview_lesson.php?&passid=63

Page 8: The Greenhouse Effect

National Aeronautics and Space Administration

At the top of the atmosphere:

+ Sunlight In – Sunlight reflected from clouds/atmosphere– Sunlight reflected from surface – IR emission 0

8

Balancing the Budget - I

http://mynasadata.larc.nasa.gov/preview_lesson.php?&passid=44

Equilibrium

Temperature: -18 °C

Page 9: The Greenhouse Effect

National Aeronautics and Space Administration 9

Balancing the Budget - II

At the Earth’s surface:

+ Sunlight absorbed – IR emission+ IR back radiation (greenhouse effect)– Thermals – Evapotranspiration 0

http://mynasadata.larc.nasa.gov/preview_lesson.php?&passid=63http://mynasadata.larc.nasa.gov/preview_lesson.php?&passid=67

Equilibrium

Temperature: 15 °C

Page 10: The Greenhouse Effect

National Aeronautics and Space Administration 10

The Enhanced Greenhouse Effect

Starting point:

Earth at equilibrium with net energy input from the Sun.

Average surface temperature 288 K (15 C; ~59 F)

Page 11: The Greenhouse Effect

National Aeronautics and Space Administration 11

The Enhanced Greenhouse Effect

The experiment:

Instantaneously double CO2 in concentration in atmosphere

Average energy emitted by Earth drops 4 W/m2 (236 vs 240)

Page 12: The Greenhouse Effect

National Aeronautics and Space Administration 12

The Enhanced Greenhouse Effect

Response:

All other things being equal, simple blackbody theory says:

Average surface temperature rises 1.2 K (or C; ~2.1 F)

Energy back in balance

Page 13: The Greenhouse Effect

National Aeronautics and Space Administration 13

The Enhanced Greenhouse Effect

Feedbacks:

In Earth system, other processes kick in (water vapor feedback, cloud feedback, ice-albedo feedback, etc).

Net effect: Average surface temperature estimated to rise 2-4.5 K (~3.6 to 8 F)

Page 14: The Greenhouse Effect

National Aeronautics and Space Administration 14

Forcings on the Greenhouse

http://ipcc.ch/publications_and_data/ar4/wg1/en/figure-spm-2.html

Page 15: The Greenhouse Effect

National Aeronautics and Space Administration

• This figure depicts mostly positive and long-lived forcing agents from 1950 through 2004. The positive forcing agents are items that cause the atmosphere to show an overall warming trend because they trap additional energy in the atmosphere (enhanced greenhouse effect). The greenhouse gasses shown in the figure (carbon dioxide - CO2, methane - CH4, halocarbons, nitrous oxide - N2O and stratospheric + tropospheric ozone - O3) have increased in the atmosphere mostly due to human activities. A natural change from variations in the Sun’s output is shown along the bottom of the graph This figure shows the cumulative effect of small changes. The additional heat trapped each year continues to add up to a warmer Earth.

Physics of Our Atmosphere 15

Energy Balance analysis

http://science-edu.larc.nasa.gov/energy_budget/

Page 16: The Greenhouse Effect

National Aeronautics and Space Administration

• Knowing how much additional heat is trapped (because we know how much of these gasses were emitted) the question becomes: where did the energy go? This figure partitions the added energy shown above based on observed changes. So far, a small amount of the energy has gone into warming the ocean – the part of the Earth that stores the most energy. Some has escaped Earth in the form of increased IR emission because of warmer temperatures. Some was reflected to space by aerosols (mostly volcanic in origin) in the stratosphere. The remainder (white band) is inferred to have been rejected due to aerosols (mostly pollution) in the troposphere, and other effects such as a changing reflection of the land surface due to deforestation, for example.

Physics of Our Atmosphere 16

Where did the Energy Go?

http://science-edu.larc.nasa.gov/energy_budget/

Page 17: The Greenhouse Effect

National Aeronautics and Space Administration 17

Interactive Applet

http://profhorn.meteor.wisc.edu/wxwise/climate/makeplanet.html

Page 18: The Greenhouse Effect

National Aeronautics and Space Administration MY NASA DATA: A REASoN Project 18