Adiabatic Lapse Rate
When 'Shallow lapse rate' is referenced it means the Environmental lapse rate is slow, or as you go up the temperature doesn't change much. A rising parcel of air will cool at approx one of the following rates: Dry (unsaturated) Adiabatic Rate is: 3ºC per 1000 ft Saturated (wet) Adiabatic Rate 1.5º per 1000 ft Standard lapse rate 1.98 per 1,000 ft The greatest determiner of wether weathering will be stable or not is the environmental lapse rate. The steeper the ELR the more unstable the weather. That is the faster it gets colder at altitude the more unstable the weather. Stable air Means Smooth flying Poor vis Steady rain Stratus Layer cloud Fog Shallow lapse rate Inversion Warm air moving over cold air Surface cooling causes stable air Radiation at night Influx of cold air (cold advection - horizontall...