Boundary Layer Height and Entrainment Zone Thickness Measured by Lidars and Wind-Profiling Radars
By S. Cohn, W. Angevine. 2000
325 citations recorded by the source corpus.
Subfields: Atmospheric Science, Environmental Engineering, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/d1f79db0163b5f1e7a592083f224456101fc5297
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Atmospheric Science
- R. Banta
- Shuyan Liu
- Xin‐Zhong Liang
- W. A. Brewer
- Philippe Drobinski
- Martial Haeffelin
- Y. Morille
- Jacques Pelon
In Environmental Engineering
- R. Banta
- Shuyan Liu
- Xin‐Zhong Liang
- W. A. Brewer
- Philippe Drobinski
- Martial Haeffelin
- Y. Morille
- Jacques Pelon
In Global and Planetary Change
- Shuyan Liu
- Xin‐Zhong Liang
- R. Banta
- Philippe Drobinski
- Martial Haeffelin
- Y. Morille
- Jacques Pelon
- D. Law
Citations in the corpus
- Determination of the Atmospheric Boundary Layer Height from Radiosonde and Lidar Backscatter (2006, background): “The height of the absolute minimum in the backscatter gradient profile is taken as the instantaneous ABL height (see also Cohn and Angevine, 1999, Davis et al., 1999; Flamant et al., 1997).”
- Doppler Lidar Estimation of Mixing Height Using Turbulence, Shear, and Aerosol Profiles (2009, methodology): “In general, most of the references use S b (range corrected) profiles to determine h A , typically assuming that the BL is characterized by higher concentrations of backscattering aerosol particles than are found above this layer in the ‘‘cleaner and drier free troposphere’’ (Cohn and Angevine 2000).”
- Observed Diurnal Cycle Climatology of Planetary Boundary Layer Height (2010, background): “Most studies have focused on algorithm development and cross validation (Marsik et al. 1995; Grimsdell and Angevine 1998; Cohn and Angevine 2000; Hennemuth and Lammert 2006; Lammert and Bösenberg 2006; Wiegner et al. 2006; Münkel et al. 2007).”
- Observations Of The Morning Transition Of The Convective Boundary Layer (2001, background): “Reflectivity (range-corrected signal-to-noise ratio) is a well-established product of wind profilers and has been shown to provide an accurate measurement of CBL height during the day (Cohn and Angevine 2000; Grimsdell and Angevine 1998; Angevine et al. 1994).”
- STRAT: An Automated Algorithm to Retrieve the Vertical Structure of the Atmosphere from Single-Channel Lidar Data (2007, methodology): “Several authors developed methods using wavelet transforms to identify particle layers in the lidar profile (e.g., Cohn and Angevine 2000; Brooks 2003), but those studies were limited to boundary layer height (BLH) analyses.”