# lab5 - Lab AOS 330 Geopotential Heights and Thickness 1...

This preview shows pages 1–2. Sign up to view the full content.

This preview has intentionally blurred sections. Sign up to view the full version.

View Full Document
This is the end of the preview. Sign up to access the rest of the document.

Unformatted text preview: Lab - AOS 330 Geopotential Heights and Thickness 1 Objectives • Learn how the hypsometric equation governs real-world pressure/height patterns. 2 Materials • Access to world-wide web • Height/thickness table (to be filled out) • Height cross-section chart • Thickness cross-section chart 3 Introduction The hypsometric equation relates the vertical spacing (“thickness”) between pairs of pressure levels to the layer mean virtual temperature. Δ Z = R d T v g ln p 1 p 2 . Horizontal temperature gradients at lower levels therefore translate into changes in pressure patterns at higher levels. An east-west jetstream at 500 hPa, for example, is the direct result of strong north-south temperature contrasts. This lab allows you to observe the relationship first-hand by analyzing data from a series of North American upper air stations. 4 Procedure 1. Go to http://weather.uwyo.edu/upperair/sounding.html 2. Set the plot type to GIF:Skew-T 3. Set the date/time to 2006 Mar 13/12Z (start)...
View Full Document

## This lab report was uploaded on 03/27/2008 for the course ATM OCN 330 taught by Professor Petty during the Fall '07 term at University of Wisconsin.

### Page1 / 2

lab5 - Lab AOS 330 Geopotential Heights and Thickness 1...

This preview shows document pages 1 - 2. Sign up to view the full document.

View Full Document
Ask a homework question - tutors are online