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The Jet Stream and Horizontal Temperature Gradients
Dramatic temperature shifts, in which warm, autumn days turn unbearably cold in what seems like minutes, are almost always ushered in by powerful winds. These temperature differences (or temperature gradients) between air masses are what actually causes the wind. This set of interactive graphs, adapted from the University of Wisconsin-Madison, allows users to control the temperature gradient between two air masses and view the effects that changes in the temperature gradient have on wind speed.
Intended for grade levels:
  • High (9-12)
  • College (13-14)
Type of resource:
  • For the classroom:
    • Computer activity
  • Visual:
    • Visualization - scientific
  • Text:
    • Ref. material
Subject:
  • Atmospheric science
Technical requirements:
Flash player
Cost / Copyright:
No cost
Copyright 2002 - 2006 WGBH Educational Foundation. All rights reserved. This site is intended for educational use only. You may not copy, reproduce, republish, upload, post, transmit, or distribute any material from this site, except that you may print out pages for use in your classroom, provided you keep intact all copyright and other proprietary notices.
DLESE Catalog ID: DLESE-000-000-009-470
Related resources:
This resource is part of 'Teacher's Domain: Jet Streams and Weather'
Resource contact / Creator / Publisher:
Publisher: WGBH Educational Foundation
Teachers' Domain
http://www.teachersdomain.org/tdhome.html