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AOS 101 Discussion 301,302,303 TA Brian Miretzky

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Why are pressure gradients around highs less then lows (upper limit to the Coriolis effect) ... Cap why is it helpful to severe storm development. Low level ... – PowerPoint PPT presentation

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Title: AOS 101 Discussion 301,302,303 TA Brian Miretzky


1
AOS 101 Discussion 301,302,303TA- Brian Miretzky
  • Class wrap-up
  • Dec. 8th-10th

2
Plan
  • Weather Discussion
  • Short Quiz
  • Up to the roof
  • Review of Exam 3 material
  • Other questions
  • Evaluations

3
Ch. 10
  • Why are pressure gradients around highs less then
    lows (upper limit to the Coriolis effect)

4
Ch. 11
  • Cap why is it helpful to severe storm
    development
  • Low level jet (nocturnal)
  • Read up on lightning
  • See rest of power from Oct. 6th-8th

5
Ch. 13
  • Different types of forecasts
  • The perfect forecast and numerical modeling

6
Ch. 14
  • Already touched some of the major issues in
    climate change lecture and climate debate

7
Ch. 15
  • Already touched some of the major issues in
    climate change lecture and climate debate

8
The end
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