Meteorology: Wave - PowerPoint PPT Presentation

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Meteorology: Wave

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Process is approximately adiabatic i.e. no external heating ... Saturated Adiabatic Lapse Rate depends on pressure and moisture content, but less than DALR. ... – PowerPoint PPT presentation

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Title: Meteorology: Wave


1
Meteorology Wave
2
The General Idea
3
Stability
As air rises and pressure falls, it expands and
cools. Process is approximately adiabatic i.e.
no external heating or cooling. Dry Adiabatic
Lapse Rate 3C/1000ft Saturated Adiabatic Lapse
Rate depends on pressure and moisture content,
but less than DALR. Potential temperature is the
temperature air would have if brought to sea
level pressure adiabatically.
4
h
?
h
?
h
?
5
Ideal Situation
6
Soundings
7
Laminar And Turbulent FlowOn Wings
8
Laminar And Turbulent FlowIn The Air
9
Synoptic Charts
  • NW Wind
  • Moderate strength
  • Straight or slightly anticyclonic isobars

10
Wind Sheer
  • Wind strength and direction varies with height
  • In general it increases and veers with height due
    to surface friction
  • Strong wind sheer tends to disrupt wave
  • Check on soundings

11
Satpics
12
Conditions For Wave
  • Suitable hills upwindgenerally NW wind
  • Stable layer
  • Moderate wind strength, typically 1520kts at
    surface
  • Increasing wind strength with height
  • Roughly constant wind direction at height
  • Straight isobars or slight anticyclonic curve
  • Luck!

13
Forecast sounding for Portmoak
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