Articles | Volume 15, issue 8
https://doi.org/10.5194/amt-15-2479-2022
https://doi.org/10.5194/amt-15-2479-2022
Research article
 | 
25 Apr 2022
Research article |  | 25 Apr 2022

Evaluating convective planetary boundary layer height estimations resolved by both active and passive remote sensing instruments during the CHEESEHEAD19 field campaign

James B. Duncan Jr., Laura Bianco, Bianca Adler, Tyler Bell, Irina V. Djalalova, Laura Riihimaki, Joseph Sedlar, Elizabeth N. Smith, David D. Turner, Timothy J. Wagner, and James M. Wilczak

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Cited articles

Adler, B., Bianco, L., Duncan, J., Turner, D. D., and Wilczak, J. M.: NOAA Microwave Radiometer Data and Thermodynamic Profile Retrievals, Version 3.0, UCAR/NCAR – Earth Observing Laboratory [data set], https://doi.org/10.26023/Y0W2-8BAG-6Y0A, last access: 30 June 2021. 
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Berg, L. K., Newsom, R. K., and Turner, D. D.: Year-long vertical velocity statistics derived from Doppler lidar data for the continental convective boundary layer, J. Appl. Meteorol., 56, 2441–2454, https://doi.org/10.1175/JAMC-D-16-0359.1, 2017. 
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Short summary
In this study, several ground-based remote sensing instruments are used to estimate the height of the convective planetary boundary layer, and their performance is compared against independent boundary layer depth estimates obtained from radiosondes launched as part of the CHEESEHEAD19 field campaign. The impact of clouds (particularly boundary layer clouds) on the estimation of the boundary layer depth is also investigated.