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In today's video, we are going to talk about Atmospheric Instability and Stability.
The Stability of the Atmosphere is the tendency of the atmosphere to promote or to suppress the vertical movement of the Air masses.
The Air masses can have different characteristics compared to the surrounding air, they can be warmer and lighter or, they can be colder and heavier.
If an Air mass is warmer than the atmosphere it will rise and cool down initially following the Dry Adiabatic Lapse Rate and, once it reaches the Dew Point it will cool down following the Saturated Adiabatic Lapse rate.
If the Environmental Lapse rate is very small, the Atmosphere will have a tendency to be stable because the Air masses will cool down faster, became heavier thus, it won't keep on climbing.
The opposite is true, if the Environmental Lapse rate is big then the mass of Air will have the tendency to be warmer and lighter thus, it will keep on climbing.
In order to understand Atmospheric Stability, we need to understand the relationship between the Environmental Lapse Rate, The Air Mass Lapse Rate.
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Timestamps:
00:00 Intro
00:45 What is Atmospheric Stability
01:00 Masses of Air Characteristics
03:55 Environmental Lapse Rate
05:00 Dry Lapse Rate
05:15 Saturated Lapse Rate
05:30 Dew Point
05:47 Atmospheric Stability Dynamics
13:35 Atmospheric Instability Dynamics
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Disclaimer:
THIS VIDEO IS FOR ENTERTAINMENT PURPOSES ONLY.
NOT FOR REAL-LIFE OPERATIONS.
PLEASE REFER TO THE OFFICIAL MANUAL AND DOCUMENTATION.
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