Articles | Volume 19, issue 2
https://doi.org/10.5194/acp-19-1129-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-19-1129-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
29 Jan 2019
Research article |
| 29 Jan 2019
| 29 Jan 2019
Long-term simulation of the boundary layer flow over the double-ridge site during the Perdigão 2017 field campaign
Johannes Wagner
CORRESPONDING AUTHOR
Deutsches Zentrum für Luft- und Raumfahrt, Institut für
Physik der Atmosphäre, 82234 Oberpfaffenhofen, Germany
Thomas Gerz
Deutsches Zentrum für Luft- und Raumfahrt, Institut für
Physik der Atmosphäre, 82234 Oberpfaffenhofen, Germany
Norman Wildmann
Deutsches Zentrum für Luft- und Raumfahrt, Institut für
Physik der Atmosphäre, 82234 Oberpfaffenhofen, Germany
Kira Gramitzky
Deutsches Zentrum für Luft- und Raumfahrt, Institut für
Physik der Atmosphäre, 82234 Oberpfaffenhofen, Germany
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Cited
23 citations as recorded by crossref.
- Multi-lidar wind resource mapping in complex terrain R. Menke et al. 10.5194/wes-5-1059-2020
- Efficacy of the Cell Perturbation Method in Large-Eddy Simulations of Boundary Layer Flow over Complex Terrain A. Connolly et al. 10.3390/atmos12010055
- Wind-Turbine and Wind-Farm Flows: A Review F. Porté-Agel et al. 10.1007/s10546-019-00473-0
- Synoptic and mesoscale winds in the complex terrain of Perdigão I. Coimbra & J. Palma 10.1088/1742-6596/2265/2/022010
- Unravelling the wind flow over highly complex regions through computational modeling and two-dimensional lidar scanning J. Palma et al. 10.1088/1742-6596/1222/1/012006
- Large-eddy simulation of wind-turbine wakes over two-dimensional hills Z. Zhang et al. 10.1063/5.0095348
- Large‐eddy simulations of the atmospheric boundary layer over an Alpine glacier: Impact of synoptic flow direction and governing processes B. Goger et al. 10.1002/qj.4263
- Nocturnal jets over wind farms in complex terrain W. Radünz et al. 10.1016/j.apenergy.2022.118959
- WRF-LES Simulation of the Boundary Layer Turbulent Processes during the BLLAST Campaign M. Udina et al. 10.3390/atmos11111149
- WindsPT e-Science platform for wind measurement campaigns D. Gomes et al. 10.1088/1742-6596/2265/2/022081
- Implications of complex terrain topography on the performance of a real wind farm F. Bernardoni et al. 10.1088/1742-6596/2505/1/012052
- Multi-scale modeling of a wind turbine wake in complex terrain B. Kale et al. 10.1088/1742-6596/2505/1/012012
- Fine-Resolution WRF Simulation of Stably Stratified Flows in Shallow Pre-Alpine Valleys: A Case Study of the KASCADE-2017 Campaign M. de Bode et al. 10.3390/atmos12081063
- Evaluation of a forest parameterization to improve boundary layer flow simulations over complex terrain. A case study using WRF-LES V4.0.1 J. Quimbayo-Duarte et al. 10.5194/gmd-15-5195-2022
- Evaluation of turbulence characteristics in WRF simulations at WiValdi wind park G. Kilroy et al. 10.1088/1742-6596/2767/5/052063
- Sensitivity of multiscale large Eddy simulations for wind power calculations in complex terrain G. De Moliner et al. 10.1016/j.apenergy.2024.123195
- Application of a new method to develop a CFD model to analyze wind characteristics for a complex terrain P. Sharma et al. 10.1016/j.seta.2019.100580
- Estimation of turbulence dissipation rate from Doppler wind lidars and in situ instrumentation for the Perdigão 2017 campaign N. Wildmann et al. 10.5194/amt-12-6401-2019
- The digital terrain model in the computational modelling of the flow over the Perdigão site: the appropriate grid size J. Palma et al. 10.5194/wes-5-1469-2020
- Bayesian Optimisation of a Two‐Turbine Configuration Around a 2D Hill Using Large Eddy Simulations C. Jané‐Ippel et al. 10.1002/we.2946
- Meso- to microscale modeling of atmospheric stability effects on wind turbine wake behavior in complex terrain A. Wise et al. 10.5194/wes-7-367-2022
- Effects of the steepness on the evolution of turbine wakes above continuous hilly terrain H. Yang et al. 10.1049/rpg2.12420
- Impact of the wind field at the complex-terrain site Perdigão on the surface pressure fluctuations of a wind turbine F. Wenz et al. 10.5194/wes-7-1321-2022
23 citations as recorded by crossref.
- Multi-lidar wind resource mapping in complex terrain R. Menke et al. 10.5194/wes-5-1059-2020
- Efficacy of the Cell Perturbation Method in Large-Eddy Simulations of Boundary Layer Flow over Complex Terrain A. Connolly et al. 10.3390/atmos12010055
- Wind-Turbine and Wind-Farm Flows: A Review F. Porté-Agel et al. 10.1007/s10546-019-00473-0
- Synoptic and mesoscale winds in the complex terrain of Perdigão I. Coimbra & J. Palma 10.1088/1742-6596/2265/2/022010
- Unravelling the wind flow over highly complex regions through computational modeling and two-dimensional lidar scanning J. Palma et al. 10.1088/1742-6596/1222/1/012006
- Large-eddy simulation of wind-turbine wakes over two-dimensional hills Z. Zhang et al. 10.1063/5.0095348
- Large‐eddy simulations of the atmospheric boundary layer over an Alpine glacier: Impact of synoptic flow direction and governing processes B. Goger et al. 10.1002/qj.4263
- Nocturnal jets over wind farms in complex terrain W. Radünz et al. 10.1016/j.apenergy.2022.118959
- WRF-LES Simulation of the Boundary Layer Turbulent Processes during the BLLAST Campaign M. Udina et al. 10.3390/atmos11111149
- WindsPT e-Science platform for wind measurement campaigns D. Gomes et al. 10.1088/1742-6596/2265/2/022081
- Implications of complex terrain topography on the performance of a real wind farm F. Bernardoni et al. 10.1088/1742-6596/2505/1/012052
- Multi-scale modeling of a wind turbine wake in complex terrain B. Kale et al. 10.1088/1742-6596/2505/1/012012
- Fine-Resolution WRF Simulation of Stably Stratified Flows in Shallow Pre-Alpine Valleys: A Case Study of the KASCADE-2017 Campaign M. de Bode et al. 10.3390/atmos12081063
- Evaluation of a forest parameterization to improve boundary layer flow simulations over complex terrain. A case study using WRF-LES V4.0.1 J. Quimbayo-Duarte et al. 10.5194/gmd-15-5195-2022
- Evaluation of turbulence characteristics in WRF simulations at WiValdi wind park G. Kilroy et al. 10.1088/1742-6596/2767/5/052063
- Sensitivity of multiscale large Eddy simulations for wind power calculations in complex terrain G. De Moliner et al. 10.1016/j.apenergy.2024.123195
- Application of a new method to develop a CFD model to analyze wind characteristics for a complex terrain P. Sharma et al. 10.1016/j.seta.2019.100580
- Estimation of turbulence dissipation rate from Doppler wind lidars and in situ instrumentation for the Perdigão 2017 campaign N. Wildmann et al. 10.5194/amt-12-6401-2019
- The digital terrain model in the computational modelling of the flow over the Perdigão site: the appropriate grid size J. Palma et al. 10.5194/wes-5-1469-2020
- Bayesian Optimisation of a Two‐Turbine Configuration Around a 2D Hill Using Large Eddy Simulations C. Jané‐Ippel et al. 10.1002/we.2946
- Meso- to microscale modeling of atmospheric stability effects on wind turbine wake behavior in complex terrain A. Wise et al. 10.5194/wes-7-367-2022
- Effects of the steepness on the evolution of turbine wakes above continuous hilly terrain H. Yang et al. 10.1049/rpg2.12420
- Impact of the wind field at the complex-terrain site Perdigão on the surface pressure fluctuations of a wind turbine F. Wenz et al. 10.5194/wes-7-1321-2022
Latest update: 20 Nov 2024
Short summary
Long-term WRF-LES simulations were performed with a horizontal resolution of 200 m for a period of 49 days during the Perdigão campaign. Simulation results were used to characterize the meteorological conditions and to analyse characteristic flow patterns. It could be shown that thermally driven flows including low-level jets frequently occurred during the observation period. Model results were in very good agreement with observations in spite of the long simulation time.
Long-term WRF-LES simulations were performed with a horizontal resolution of 200 m for a period...
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