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
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?