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“A Globe Walk” Modeling the “Reasons for the Seasons”

“A Globe Walk” Modeling the “Reasons for the Seasons”. “Models are tentative schemes or structures that correspond to real objects, events, or classes of events, and that have explanatory power…….” The National Science Education Standards (Page 117); National Academy Press 1998.

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“A Globe Walk” Modeling the “Reasons for the Seasons”

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  1. “A Globe Walk” Modeling the “Reasons for the Seasons”

  2. “Models are tentative schemes or structures that correspond to real objects, events, or classes of events, and that have explanatory power…….” The National Science Education Standards (Page 117); National Academy Press 1998.

  3. Earth Rotates on Its Axis Earth is Tilted on its Axis Earth’s Revolves in an Orbit around the Sun Earth’s Orbital Radius is Constantly Changing. The Lengths of Daytimes Gradually Change as the Seasons Change. The Altitudes of the Sun Gradually Change during a Day and as the Seasons Change. Seasonal changes are most dramatic in the Polar Regions. A Class of Events

  4. Most students are aware of seasonal changes in lengths of daytime but may not know that they depend on Latitude. http://www.eoearth.org/article/Earth-Sun_relationships_and_insolation

  5. Today, the “midday” altitude of the sun in Kotzebue, Alaska is 44.8º at 1:55 PM Alaska Standard Time. The Distant Horizon A U.S. Naval Observatory web site provides the sun’s altitude on any day at any Latitude . Students are probably less aware of seasonal changes in the “altitude” of the sun. http://www.usno.navy.mil/USNO/astronomical-applications/data-services/alt-az-us

  6. You can learn more about Kotzebue by visiting their web site. Kotzebue, Alaska is located 33 miles north of the Arctic Circle http://kotzpdweb.tripod.com/city/index.html

  7. The Distant Horizon A U.S. Naval Observatory web site provides the sun’s altitude on any day at any Latitude . Today, the “midday” altitude of the sun in Amherst is 69.4º at 11:50 AM Eastern Standard Time. http://www.usno.navy.mil/USNO/astronomical-applications/data-services/alt-az-us

  8. Diagrams have limited value illustrating seasonal changes in the altitude of the sun and lengths of daytime http://okfirst.mesonet.org/train/meteorology/Seasons.html

  9. Animations can more effectively reveal aspects of seasonal changes such as the lengths of daytimes in the Polar Regions. http://www.cs.sbcc.cc.ca.us/~physics/flash/LengthofDay.swf http://esminfo.prenhall.com/science/geoanimations/animations/01_EarthSun_E2.html

  10. A classroom, a model of the sun, a model of Earth, a representation of Earth’s orbit, two straws, and a protractor can be used to demonstrate a variety of daily and seasonal changes. The Globe Walk

  11. The 2010 Astronomical Seasons (for the Northern Hemisphere) Spring began at 12:32 PM EST on March 20th Summer began at 6:28 AM EST on June 21st Autumn will begin at 10:09 EST on September 21st\ Winter will begin at 6:38 PM EST on December 21st A Demonstration ofSolstices and Equinoxes

  12. Changes in the altitude of the sun at different Latitudes as the seasons change. Changes in the Lengths of Daytimes at different Latitudes as the seasons change. Summer Solstice at the North Pole. Daily changes in the Altitude of the Sun. Other Globe Walk Demonstrations Include:

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