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Observed Structure of the Atmospheric Boundary Layer Many thanks to: Nolan Atkins, Chris Bretherton, Robin Hogan
Review of the last lecture ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Vertical Structure of the Atmosphere ,[object Object],[object Object]
Difference between boundary layer and free atmosphere ,[object Object],[object Object],[object Object],[object Object],[object Object]
Vertical structure of the boundary layer ,[object Object],[object Object],[object Object],[object Object],[object Object]
Turbulence inside the boundary layer ,[object Object]
Generation of turbulence in the boundary layer: Hydrodynamic instability ,[object Object],[object Object],[object Object]
Shear instability ,[object Object]
Example: Kelvin-Helmholtz instability ,[object Object],Lab experiment Real world  (K-H clouds)
Convective instability ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],Stable or  sub-adiabatic Neutral or adiabatic Unstable or super-adiabatic
Forcings generating  temperature gradience and wind shear,  which affect the boundary layer depth ,[object Object],[object Object]
Boundary layer depth: Effects of ocean and land ,[object Object],[object Object]
Boundary layer depth: Effect of highs and lows ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Boundary Layer depth: Effects of diurnal forcing over land ,[object Object],[object Object]
Convective mixed layer (CML): Growth ,[object Object]
Convective mixed layer (CML): Vertical profiles of state variables ,[object Object],Super-adiabatic Nearly adiabatic Strongly stable lapse rate
Nocturnal boundary layer over land:  Vertical structure ,[object Object],[object Object],Strongly stable lapse rate Nearly adiabatic Weakly stable lapse rate
Boundary layer over land:  Comparison between day and night ,[object Object],Kaimal and Finnigan 1994 Super-adiabatic Nearly adiabatic Strongly stable lapse rate Strongly stable lapse rate Nearly adiabatic Weakly stable lapse rate
Summary ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]

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Atmospheric Boundary Layer Structure Observations Review

  • 1. Observed Structure of the Atmospheric Boundary Layer Many thanks to: Nolan Atkins, Chris Bretherton, Robin Hogan
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