Dynamics of the Atmospheric Boundary Layer over two middle-latitude rural sites with Doppler lidar
Metadatos
Afficher la notice complèteAuteur
Ortiz Amezcua, Pablo; Andújar Maqueda, Juana; Benavent Oltra, José Antonio; Casquero Vera, Juan Andrés; Alados Arboledas, Lucas; Guerrero Rascado, Juan LuisEditorial
Elsevier
Materia
Doppler lidar Wind Turbulence Rural boundary layer Olive orchard Peatland
Date
2022-09-08Referencia bibliográfica
Pablo Ortiz-Amezcua... [et al.]. Dynamics of the Atmospheric Boundary Layer over two middle-latitude rural sites with Doppler lidar, Atmospheric Research, Volume 280, 2022, 106434, ISSN 0169-8095, [https://doi.org/10.1016/j.atmosres.2022.106434]
Patrocinador
Fundacion Ramon Areces; European Space Agency 4000119961/16/NL/FF/mg; Polish National Science Centre (NCN) 2021/40/C/ST10/00023; Spanish Government CGL2015-73250-JIN CGL201681092-R CGL2017-83538-C3-1-R CGL2017-90884-REDT PID2020117825GB-C21 PID2020-120015RB-100; Andalusian Regional Government P18-RT-3820; FEDER-UGR program ARNM-430-UGR20; University of Granada; ACTRIS-2 Research Infrastructure Project of the European Union's Horizon 2020 research and innovation program 654109; European Cooperation in Science and Technology (COST) CA18235; Universidad de Granada/CBUARésumé
The Atmospheric Boundary Layer (ABL) over two middle-latitude rural sites was characterized in terms of mean
horizontal wind and turbulence sources using a standard classification methodology based on Doppler lidar. The
first location was an irrigated olive orchard in Úbeda (Southern Spain), representing one of the most important
crops in the Mediterranean basin and a typical site with Mediterranean climate. The second location was PolWET
peatland site in Rzecin (Northwestern Poland), representing one of the largest natural terrestrial carbon storages
that have a strong interaction with the climate system. The results showed typical situations for non cloud-topped
ABL cases, where ABL is fully developed during daytime due to convection, with high turbulent activity and
strong positive skewness indicating frequent and powerful updrafts. The cloud-topped cases showed the strong
influence that clouds can have on ABL development, preventing it to reach the same maximum height and
introducing top-down movements as an important contribution to mixing. The statistical analysis of turbulent
sources allowed for finding a common diurnal cycle for convective mixing at both sites, but nocturnal wind shear
driven turbulence with marked differences in its vertical distribution. This analysis demonstrates the Doppler
lidar measurements and the classification algorithm strong potential to characterize the dynamics of ABL in its
full extent and with high temporal resolution. Moreover, some recommendations for future improvement of the
classification algorithm were provided on the basis of the experience gained.