Articles | Volume 19, issue 17
https://doi.org/10.5194/amt-19-5697-2026
https://doi.org/10.5194/amt-19-5697-2026
Research article
 | 
08 Sep 2026
Research article |  | 08 Sep 2026

Modelling monthly Boundary Layer Height maps combining radiosonde, satellite, and reanalysis over Europe

Carina I. Argañaraz, Andreu Salcedo-Bosch, Simone Lolli, and Gabriele Curci

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Cited articles

Argañaraz, C. I., Salcedo-Bosch, A., Lolli, S., and Curci, G.: Building a high-resolution climate gridded dataset in complex terrain: validating different methods in Abruzzo region in Italy, Int. J. Climatol., 0, e70153, https://doi.org/10.1002/joc.70153, 2025. 
Ayazpour, Z., Tao, S., Li, D., Scarino, A. J., Kuehn, R. E., and Sun, K.: Estimates of the spatially complete, observational-data-driven planetary boundary layer height over the contiguous United States, Atmos. Meas. Tech., 16, 563–580, https://doi.org/10.5194/amt-16-563-2023, 2023. 
CariArgBio: CariArgBio/Modelling-monthly-Boundary-Layer-Height-maps-combining-different-data-sources: Modelling monthly Boundary Layer Height maps combining different data sources (Version kriging), Zenodo [computer software], https://doi.org/10.5281/zenodo.22232601, 2026. 
Cavalleri, F., Viterbo, F., Brunetti, M., Bonanno, R., Manara, V., Lussana, C., Lacavalla, M., and Maugeri, M.: Inter-comparison and validation of high-resolution surface air temperature reanalysis fields over Italy, Int. J. Climatol., 44, 2681–2700, https://doi.org/10.1002/joc.8475, 2024. 
Chen, X., Yang, T., Wang, Z., Wang, F., and Wang, H.: An ensemble method for improving the estimation of planetary boundary layer height from radiosonde data, Atmos. Meas. Tech., 16, 4289–4302, https://doi.org/10.5194/amt-16-4289-2023, 2023. 
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Short summary
In this study, maps of the planetary boundary layer over Europe were generated by integrating multiple data sources. The results show higher accuracy compared with the widely used ERA5 reanalysis. The proposed regression kriging method performed well in estimating the height of the boundary layer at 12:00 UTC, and to a lesser extent at 00:00 UTC.
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