Lapse rates
Standard lapse rate: 2°C per 1000 feet
Dry adiabatic lapse rate: 3°C per 1000 feet
Moist adiabatic lapse rate: 1.1-2.8°C per 1000 feet
Standard pressure lapse rate: 1” per 1000 feet
What is necessary for cloud formations
Condensation nuclei
Moisture
Small temperature/dew point spread
Standard temperature and pressure
29.92 inches of mercury at sea level
14.7 psi
1014 millibars
15°C
High pressure system
Low pressure system
Temperature inversion
Temperature increases with altitude in layers.
Stable air below layer, unstable (turbulence) below layer.
Low Clouds
Middle Clouds
High Clouds
EVD Clouds
2. Very unstable and turbulence
Fog formation
Fog is formed by adding moisture to the air and reducing the temperature to dew point.
Temperature / dew point
When temp and dew point are equal, a parcel of air can no longer hold water and visible moisture occurs.
Stable air
Cool dry air (Arctic)
V) poor C) stratus T) little to none I) rime ice P) steady P) high