Title: Meteorology: Wave
1Meteorology Wave
2The General Idea
3Stability
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.
4h
?
h
?
h
?
5Ideal Situation
6Soundings
7Laminar And Turbulent FlowOn Wings
8Laminar And Turbulent FlowIn The Air
9Synoptic Charts
- NW Wind
- Moderate strength
- Straight or slightly anticyclonic isobars
10Wind 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
11Satpics
12Conditions 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!
13Forecast sounding for Portmoak