Articles | Volume 19, issue 7
https://doi.org/10.5194/acp-19-4615-2019
© 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-19-4615-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
From weak to intense downslope winds: origin, interaction with boundary-layer turbulence and impact on CO2 variability
Departamento de Física de la Tierra y Astrofísica, Universidad Complutense de Madrid, Madrid, Spain
Invited contribution by Jon Ander Arrillaga, recipient of the EGU Nonlinear Processes in Geosciences Outstanding Student Poster Award 2015.
Carlos Yagüe
Departamento de Física de la Tierra y Astrofísica, Universidad Complutense de Madrid, Madrid, Spain
Carlos Román-Cascón
Departamento de Física de la Tierra y Astrofísica, Universidad Complutense de Madrid, Madrid, Spain
Laboratoire d'Aérologie, CNRS, Université de Toulouse, CNRS, UPS, Toulouse, France
Mariano Sastre
Departamento de Física de la Tierra y Astrofísica, Universidad Complutense de Madrid, Madrid, Spain
Maria Antonia Jiménez
Departament de Física, Universitat de les Illes Balears, Palma, Spain
Gregorio Maqueda
Departamento de Física de la Tierra y Astrofísica, Universidad Complutense de Madrid, Madrid, Spain
Jordi Vilà-Guerau de Arellano
Meteorology and Air Quality Group, Wageningen University, Wageningen, the Netherlands
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- The unexpected high frequency of nocturnal surface ozone enhancement events over China: characteristics and mechanisms C. He et al. 10.5194/acp-22-15243-2022
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- Types of Vertical Structure of the Nocturnal Boundary Layer L. Mahrt & O. Acevedo 10.1007/s10546-022-00716-7
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Latest update: 31 Mar 2025
Short summary
Thermally driven downslope winds develop in mountainous areas under a weak large-scale forcing and clear skies. In this work, we find that their onset time and intensity are closely connected with both the large-scale wind and soil moisture. We also show how the distinct downslope intensities shape the turbulent and thermal features of the nocturnal atmosphere. The analysis concludes that the downslope–turbulence interaction and the horizontal transport explain the important CO2 variability.
Thermally driven downslope winds develop in mountainous areas under a weak large-scale forcing...
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