Example Lesson - Relating IR Temperature Derived from Satellites to Cloud
Top Heights
Michael R. Taber
3010 Agronomy Hall
Iowa State University
Ames, Iowa 50011 mtaber@iastate.edu
Office hours: 2-4 PM
Objective
Upon completion of module, the student will have
a basic understanding of the relationship between remotely sensed
Infrared Temperature (IR) and the height of cloud tops.
Students will complete a concept map in order to synthesize the
lesson concepts.
Statement of the Problem
When looking at an IR satellite image, how can we tell the height of the
cloud tops, particularly for thunderstorms?
Procedure
You should keep notes while working on the "Exploration" section. You
are only required to turn in your responses to the "Evaluation"
and "Summary" sections.
Further exploration
Once you understand the basics of IR satellite image and the relationship to
cloud height, you might want to explore how visible and water vapor satellite
images can be used in furthering your understanding of cloud development. Once
again, visit UIUC's Online
guide to satellite imagery, "Visible vs. Infrared vs. Water
Vapor."
In this section, think about the IR satellite map from UIUC. What do the darker
areas represent? Look in southern California in the vicinity of the Mojave
Desert. Do you see dark or bright areas? Think about the likely surface temperature in
the Mojave Desert. Now, what do the darker areas on the Satellite map likely
represent, a warmer or colder surface?