- 1Universidad Complutense de Madrid, Facultad de Ciencias Fisicas, Fisica de la Tierra y Astrofisica, Spain (pabloo01@ucm.es)
- 2Departamento de Física Aplicada, Facultad de Ciencias del Mar y Ambientales, INMAR, CEIMAR, Universidad de Cádiz, Puerto Real, Spain
- 3Laboratorie d’Aerologie, CNRS, Université de Toulouse, 31400 Toulouse, France
- 4NorthWest Research Associates, Boulder, Colorado, United States of America
Nocturnal downvalley flows were examined in a valley located in southern France, near the Pyrenees. Three meteorological stations were strategically placed at different locations within the valley, collecting a year-long dataset of near-surface observations. This dataset enables an investigation of how these flows are organized and evolve throughout the annual cycle.
To identify the downvalley flow events, we applied a breeze detection algorithm (Arrillaga et al., 2018; Román-Cascón et al., 2019). Once detected, the events were characterized in terms of onset, peak intensity, and duration, with particular attention paid to the synoptic conditions conducive to their development. A clustering approach was also employed to classify and compare subtypes of breeze days, providing insights into their controlling factors and distinctive features.
Furthermore, a statistical analysis differentiating various turbulence regimes (incorporating HOckey STick (HOST) analysis) offers a deeper understanding of how turbulence interacts with flow dynamics. Overall, this work seeks to advance our knowledge of the mechanisms driving thermally-driven flows in complex terrain over a full annual cycle.
How to cite: Ortiz-Corral, P., Román-Cascón, C., Jiménez-Rincon, J. A., Lohou, F., Lothon, M., Sastre, M., Sun, J., and Yagüe, C.: Statistical Analysis of Nocturnal Downvalley Flows Over the Annual Cycle: Insights from a Pyrenean Valley (France), EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-16689, https://doi.org/10.5194/egusphere-egu25-16689, 2025.