| Issue |
EPJ Web Conf.
Volume 362, 2026
31st International Laser Radar Conference (ILRC 31) Held Together with the 22nd Coherent Laser Radar Conference (CLRC 22)
|
|
|---|---|---|
| Article Number | 06014 | |
| Number of page(s) | 4 | |
| Section | Joint CLRC/ILRC Session: Flux Measurements and Boundary Layer Dynamics | |
| DOI | https://doi.org/10.1051/epjconf/202636206014 | |
| Published online | 09 April 2026 | |
https://doi.org/10.1051/epjconf/202636206014
Turbulent coherent structures in the atmospheric surface layer: A 13-month study of dynamics based on Doppler lidar observations in mid-latitude coastal city
Laboratory of Physico-Chemistry of the Atmosphere (LPCA), UR 4493, University of the Littoral Opal Coast (ULCO), Dunkirk, France.
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Published online: 9 April 2026
Abstract
Turbulent coherent structures such as streaks play a crucial role in turbulent flows' behavior and pollutants' dispersion in the surface layer. This research is based on ~40,000 horizontal Doppler lidar scans recorded during a 13-month campaign in Dunkirk, France, an industrial harbor city on the North Sea. Similarly to Cheliotis et al. [1], this work is based on the results of automated classification, detailed in a companion abstract. This approach which is based on texture analysis and supervised machine learning, facilitated the distinction between organized and disorganized streaks, which appeared, respectively, mainly during the day and at dawn and dusk. There was no significant seasonal variation in the appearance of the two streak types, beyond the fact it followed the sunrise and sunset times. Organized streaks were typically associated with neutral to unstable atmospheric conditions and characterized by higher motion and thermal fluxes than their disorganized counterparts. Conversely, disorganized structures were more narrowly associated with stable conditions and higher friction velocity. The classification parameters also allowed retrieving the streaks' direction misalignment with the mean wind and their periodicity. The misalignment was more pronounced for disorganized streaks and varied between 0 and 20°. Organized streaks tended to be slightly narrower than disorganized ones, with periods of 0.48 ± 0.22 km and 0.42 ± 0.25 km, respectively (average ± 1σ standard deviation). The aspect ratio of streaks (width-to-height ratio) could only be determined during a few night-time case studies, due to difficulties in differentiating the surface and mixed layers using Doppler lidar data only. The retrieved aspect ratio of 1.64, therefore, corresponds to disorganized streaks.
© The Authors, published by EDP Sciences, 2026
This is an Open Access article distributed under the terms of the Creative Commons Attribution License 4.0, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.
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