Observed Diurnal Cycle Climatology of Planetary Boundary Layer Height

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Convective Boundary Layer Heights Over Mountainous Terrain—A Review of Concepts (2015, background): “, 1988 ; Liu and Liang , 2010 ) and show a variety of CBL height behaviors , from terrain - following to more level CBL heights .”
Climatology of the planetary boundary layer over the continental United States and Europe (2012, background): “Second, there are no climatological (large space and time scale) observational analyses of the PBL, mainly because of the lack of direct measurements of PBL height and of suitable measurements that could be used to estimate it [Liu and Liang, 2010].”
On the computation of planetary boundary-layer height using the bulk Richardson number method (2014, methodology): “where δ is the minimumH for unstable conditions, which, in practice, is specified as a small positive value instead of zero (Liu and Liang, 2010).”
A Planetary Boundary Layer Height Climatology Derived from ECMWF Reanalysis Data (2013, methodology): “We estimate it based on PBL height data fromLiu and Liang (2010), collected at theAtmospheric Radiation Measurement Program (ARM) Southern Great Plains site.”