DOC PREVIEW
UNC-Chapel Hill GEOG 111 - Wave Cyclones

This preview shows page 1 out of 2 pages.

Save
View full document
Premium Document
Do you want full access? Go Premium and unlock all 2 pages.
Access to all documents
Download any document
Ad free experience

Unformatted text preview:

GEOG 111 1st Edition Lecture 27 Outline of Last Lecture I Snow a Significance b Formation c Atmospheric patterns Outline of Current Lecture I Wave cyclones a Where do they occur Current Lecture I Wave cyclones a Where do they occur i Along a front where there is a temperature gradient ii Fronts encourage the lifting of air clouds and precipitation iii Middle troposphere around cold front is much colder 1 The ELR tends to be steeper 2 Unstable conditions stronger lifting thicker clouds and heavier precipitation iv Beneath the jet stream aloft and downstream of a trough 1 Rising air equates with area of upper level divergence a Occurs just downstream from trough 2 Air is slowing down creating upper level convergence sinking air motions causing high pressure at surface a Occurs upstream from trough v Know this diagram well for test 3 These notes represent a detailed interpretation of the professor s lecture GradeBuddy is best used as a supplement to your own notes not as a substitute


View Full Document

UNC-Chapel Hill GEOG 111 - Wave Cyclones

Documents in this Course
Load more
Download Wave Cyclones
Our administrator received your request to download this document. We will send you the file to your email shortly.
Loading Unlocking...
Login

Join to view Wave Cyclones and access 3M+ class-specific study document.

or
We will never post anything without your permission.
Don't have an account?
Sign Up

Join to view Wave Cyclones and access 3M+ class-specific study document.

or

By creating an account you agree to our Privacy Policy and Terms Of Use

Already a member?