The Alaiz experiment: untangling multi-scale stratified flows over complex terrain
Autor: | Javier Sanz Rodrigo, Joan Cuxart, Jakob Mann, Belén Martí, Fernando Borbón, Nikola Vasiljevic, Pedro A. Santos, Daniel Martínez-Villagrasa, Elena Cantero |
---|---|
Jazyk: | angličtina |
Rok vydání: | 2020 |
Předmět: |
010504 meteorology & atmospheric sciences
Scale (ratio) Renewable Energy Sustainability and the Environment Flow (psychology) lcsh:TJ807-830 Stratified flows lcsh:Renewable energy sources Energy Engineering and Power Technology Terrain 15. Life on land Geodesy 01 natural sciences 010305 fluids & plasmas symbols.namesake Cross section (physics) Lidar 0103 physical sciences Froude number symbols Hydraulic jump Geology 0105 earth and related environmental sciences |
Zdroj: | Wind Energy Science, Vol 5, Pp 1793-1810 (2020) Santos, P, Mann, J, Vasiljević, N, Cantero, E, Sanz Rodrigo, J, Borbón, F, Martínez-Villagrasa, D, Martí, B & Cuxart, J 2020, ' The Alaiz experiment: Untangling multi-scale stratified flows over complex terrain ', Wind Energy Science, vol. 5, no. 4, pp. 1793-1810 . https://doi.org/10.5194/wes-5-1793-2020 |
ISSN: | 2366-7451 2366-7443 |
Popis: | We present novel measurements from a field campaign that aims to characterize multi-scale flow patterns, ranging from 0.1 to 10 km in a time-resolved manner, in a mountainous region in northwestern Spain with a mountain–valley–ridge configuration. We select two flow cases where topographic-flow interactions were measured by five synchronized scanning Doppler wind lidars along a 10 km transect line that includes a cross section of the valley. We observed a hydraulic jump in the lee side of the mountain. For this case, the Froude number transition from supercritical (>1) at the mountain to subcritical () at the valley is in agreement with previous experiments at a smaller scale. For a 1-year period, the measurements show such a transition about 10 % of the time, indicating a possible high occurrence of hydraulic jumps. The second flow case presents valley winds that are decoupled from the northerly flow aloft and show a stratified layered pattern, which is well captured by the lidar scans and complementary ground-based observations. These measurements can aid the evaluation of multi-scale numerical models as well as improve our knowledge with regards to mountain meteorology. |
Databáze: | OpenAIRE |
Externí odkaz: |