Articles | Volume 17, issue 6
https://doi.org/10.5194/amt-17-1679-2024
https://doi.org/10.5194/amt-17-1679-2024
Research article
 | 
25 Mar 2024
Research article |  | 25 Mar 2024

CALOTRITON: a convective boundary layer height estimation algorithm from ultra-high-frequency (UHF) wind profiler data

Alban Philibert, Marie Lothon, Julien Amestoy, Pierre-Yves Meslin, Solène Derrien, Yannick Bezombes, Bernard Campistron, Fabienne Lohou, Antoine Vial, Guylaine Canut-Rocafort, Joachim Reuder, and Jennifer K. Brooke

Data sets

UHF-RADAR - P2OA-CRA station - Level 2A wind profiles - Monthly files M. Lothon https://doi.org/10.25326/563

LA Site 1 F. Saïd https://doi.org/10.6096/bllast.uhf.site1

LIAISE ELS-PLANS LAERO UHFWindProfiler-LowMode L2 M. Lothon and A. Vial https://doi.org/10.25326/363

UHF CNRM Site 2 O. Garrouste https://doi.org/10.6096/bllast.uhf.site2

LIAISE LA-CENDROSA CNRM UHFWindProfiler-LowMode L2 M. Lothon https://doi.org/10.25326/471

P2OA-CRA station - Turbulence measurements - L2A F. Lohou et al. https://doi.org/10.25326/550

60 m Tower - P2OA-CRA station - Meteorological variables - L2A F. Lohou et al. https://doi.org/10.25326/551

Meteorological parameters and flux F. Lohou https://doi.org/10.6096/bllast.60mtower.meteo

LIAISE ELS-PLANS UKMO MTO-30MIN L2 J. Price https://doi.org/10.25326/430

LIAISE LA-CENDROSA CNRM MTO-1MIN L2 G. Canut https://doi.org/10.25326/33

MODEM Radiosoundings Site 1 M. Lothon https://doi.org/10.6096/bllast.modem

Frequent radiosoundings Site 2 D. Legain https://doi.org/10.6096/bllast.frequentsoundingssite2

LIAISE ELS-PLANS UKMO radiosondes L1 J. Price https://doi.org/10.25326/429

LIAISE LA-CENDROSA CNRM RS L2 O. Garrouste https://doi.org/10.25326/322

SUMO J. Reuder and M. Jonassen https://doi.org/10.25326/469

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Short summary
We present a new algorithm, CALOTRITON, for the retrieval of the convective boundary layer depth with ultra-high-frequency radar measurements. CALOTRITON is partly based on the principle that the top of the convective boundary layer is associated with an inversion and a decrease in turbulence. It is evaluated using ceilometer and radiosonde data. It is able to qualify the complexity of the vertical structure of the low troposphere and detect internal or residual layers.