Lesson 1 Introduction
Lesson 2
Station Plotting-Decoding and Cloud Types
Lesson 3
Contouring I
Lesson 4
Contouring II
Lesson 5
Air Masses
Lesson 6
Fronts
Lesson 7
Satellite
Lesson 8
Radar and Thunderstorms
Lesson 9
Upper Air
Lesson 10
Mid-Latitude Cyclone
Lesson 11
Case Study I
Lesson 12
Case Study II

Upper Air Maps

Here is an 500 mb upper air map. The height contours are in blue and the red dotted lines are temperature. Notice, that high heights are associated with warmer air.

It is important to identify the troughs and ridges on these upper air maps.

Here is an example of the relationship between the weather at the surface and the flow of air at middle levels of the atmosphere. In particular, note the position of the cold front and low pressure system at the surface on the west coast. Is this under a trough or a ridge when viewing the upper air map at 500 mb? Also notie the upper level ridge of the 500 mb map that is over the central US (i.e. Nebraska, Kansas, Iowa, etc.) and the weather at the surface. Do notice a relationshipt between the cloudiness beneath the ridge?

Now make observations about the relationship between the weather at the surface and the flow at 300 mb.

Also note the relationship between the upper air troughs and the infrared satellite image.

Return to upper air map lesson.

Return to Lab 101 Main Page

Local Madison Weather



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) 1999 by Steve Ackerman .  Feel free to use this material for non-profit educational purposes!