Chapter 6 - Stability and Cloud Development
Index of Lecture Notes
introduction to cloud development and atmospheric stability
the concept of stability
the concept of instability
introduction to atmospheric stability
the bottom line for rising/sinking parcels
rising air parcel - adiabatic cooling
sinking air parcel - adiabatic warming
dry adiabatic lapse rate:
ascending unsaturated parcel at surface
temp at 1km
temp at 2km - it saturates
moist adiabatic lapse rate:
temp at 3 km - saturated parcel
temp at 4 km
dry versus moist adiabatic processes
Different Stability Cases:
absolute stability
inversion layers
how to form stable layers
subsidence inversions
absolute instability
conditional instability
conditional instability - example - surface
conditional instability - example - 1 km
conditional instability - example - 2 km
conditional instability - example - 3 km
conditional instability - example - 4 km
conditional instability - example - 5 km
assessing the stability of the environment
methods to destabilize the environment
methods to destabilize the environment, cont
stability and observed cloud development - what determines cloud base and cloud top?
stability and observed cloud development - what determines cloud base and cloud top - example
Interactive sounding illustrating cloud development
lifting mechanisms - introduction
convection
stable environment
shallow conditionally unstable environment
deep conditionally unstable environment
topographical lifting
wave clouds
frontal lifting
convergence
Review Questions
SAMPLE TEST QUESTIONS FOR CH 6
CH 7 HOMEWORK:
NOTES
|
PROBLEMS