Lesson 1
Chapters 1 & 2
Lesson 2
Chapter 3 & Instrument Supplement
Lesson 3
Weather Maps
Lesson 4
Chapter 4
Lesson 5
Chapter 5
Lesson 6
Chapter 6
Lesson 7
Chapter 7
Lesson 8
Chapter 8
Lesson 9
Chapter 9
Lesson 10
Chapter 10
Lesson 11
Wind Shear and Turbulence
Lesson 12
Icing
Lesson 13
Visibility
Lesson 14
Case Study/Self-Briefing
Lesson 15
Case Study/Self-Briefing
Lesson 16
Case Study/Self-Briefing

FRONTS PRACTICE

The Contour Applet for Fronts

Fronts are given their name because they are the battle zone between two different air masses. They can be identified by any of the following characteristics: a sharp temperature gradient, a sharp moisture gradient, or a sharp change in wind direction. Fronts are categorized according to their net movement. For example, when a warm air mass advances on a cooler air mass, the boundary between them is called a warm front. Clouds and light to moderate precipitation usually form ahead of a warm front. When a cold air mass advances on a warmer air mass, the boundary is called a cold front. Since surface friction creates a much steeper slope in a cold front than in a warm front, air masses are lifted more rapidly and clouds grow to greater vertical extent. A narrow but heavy band of precipitation is usually seen along a cold front.

Practice Drawing Fronts and Highs/Lows

(Copyright 1999, University of Wisconsin-Madison/SSEC)

Across the top of the drawing region are a series of buttons:

  • Erase Last Line - This button erases the lastest line you've drawn. Hitting this button twice will erase the last two lines (or letters) you drew.
  • Objects - Use this to select the type of front or pressure center you want to draw. Just select one of these and then 'drag' the mouse on the image below (that is, press and hold the mouse button while moving the pointer).

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This web based lab section is being developed with assistance from the College of Letters and Science and the Cooperative Institute of Meteorological Satellite Studies.   Material presented is Copyrighted (C) 2000 by Steve Ackerman .  Feel free to use this material for non-profit educational purposes!