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Upwelling Terrestrial Radiation
The Stefan-Boltzmann Law is a fundamental law of physics. In this lesson, students will use this law and the near-ground air temperature to compute the hourly irradiance emitted by the surface of Earth. Then comparisons will be made with actual observations of this variable, called upwelling terrestrial radiation.
Intended for grade levels:
  • High (9-12)
Type of resource:
  • For the classroom:
    • Lab activity
    • Lesson plan
Subject:
  • Atmospheric science
  • Physics
Technical requirements:
No specific technical requirements, just a browser required
Cost / Copyright:
No cost
Copyright 2005 Board of Regents of the University of Oklahoma. All Rights Reserved.
DLESE Catalog ID: DLESE-000-000-008-759
Educational standards:
  • National Science Education Standards (NSES):
    • 9-12:
      • Unifying concepts and processes:
        • Evidence, models, and explanation
      • B - Physical science:
        • Interactions of energy and matter
      • D - Earth and space science:
        • Energy in the earth system
      • E - Science and technology:
        • Understandings about science and technology
Resource contact / Creator / Publisher:
Publisher: Oklahoma Climatological Survey
EarthStorm Educational Outreach
http://earthstorm.ocs.ou.edu/default.php

Contact: Andrea Melvin
EarthStorm
Oklahoma Climatological Survey