Determination of the Atmospheric Boundary Layer Height from Radiosonde and Lidar Backscatter

By B. Hennemuth, A. Lammert. 2006

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Observed Diurnal Cycle Climatology of Planetary Boundary Layer Height (2010, background): “Nonetheless, our comparison reaches a conclusion similar to Hennemuth and Lammert (2006), who found that the PBLH based on radisonde and lidar data deviates between 6200 m.”
Doppler Lidar Estimation of Mixing Height Using Turbulence, Shear, and Aerosol Profiles (2009, methodology): “The data provided by these radiosondes were used to derive u proﬁles that were used with the corresponding RH proﬁle to hand-pick the MH based on the gradient method (Hennemuth and Lammert 2005; Martucci et al. 2007).”
Climatology of the planetary boundary layer over the continental United States and Europe (2012, methodology): “, 2006; van der Kamp and McKendry, 2010], lidar [Hennemuth and Lammert, 2006; Tucker et al., 2009], wind-profiling and boundary layer radar [Angevine et al.”
Convective Boundary Layer Heights Over Mountainous Terrain—A Review of Concepts (2015, unknown): “Several studies over flat terrain have shown a good correspondence between estimates of the CBL height from lidar and temperature profiles (Coulter, 1979; Van Pul et al., 1994; Marsik et al., 1995; Hayden et al., 1997; Hennemuth and Lammert, 2006) with maximum differences on the order of a few hundr”