REVIEW
QUESTIONS FOR CH10- WIND: SMALL-SCALE AND LOCAL SYSTEMS
- How are global, synoptic, mesoscale, and
microscale motions defined spatially and temporally?
- What common atmospheric phenomena occur on
each of these scales?
- How well can we forecast weather events on
each of these scales?
- What are the common types of friction in
the boundary layer and how are they created?
- How is turbulence generated?
- How does the boundary layer evolve during
the course of a day?
- What does turbulence intensity depend
upon?
- How are small-scale eddies formed in the
atmosphere?
- How is CAT formed?
- Why are winds at the top of mountain, or
through mountain passes often quite strong?
- How are winds measured?
- What is a wind rose and how is it
interpreted?
- How do thermal circulations form? What are
the fundamental processes involved (very important!!!)?
- What are common examples of thermal
circulations? How deep are they?
- What changes can one experience with
sea-breeze frontal passage?
- How are winds affected by moving over
surfaces with different frictional characteristics?
- How do valley and mountain (upslope) winds
form?
- How do katabatic winds form?
- How do chinook winds form?
- How do Santa Ana winds form?
- How does a Haboob form?
last updated:
08/20/04 10:04 AM