Articles | Volume 15, issue 15
https://doi.org/10.5194/acp-15-9031-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/acp-15-9031-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
14 Aug 2015
Research article |
| 14 Aug 2015
Interactions among drainage flows, gravity waves and turbulence: a BLLAST case study
Dept. de Geofísica y Meteorología, Universidad Complutense de Madrid, Madrid, Spain
Dept. de Geofísica y Meteorología, Universidad Complutense de Madrid, Madrid, Spain
L. Mahrt
NorthWest Research Associates, Corvallis, OR, USA
M. Sastre
Dept. de Geofísica y Meteorología, Universidad Complutense de Madrid, Madrid, Spain
G.-J. Steeneveld
Meteorology and Air Quality Section, Wageningen University, Wageningen, the Netherlands
E. Pardyjak
Department of Mechanical Engineering, University of Utah, Salt Lake City, UT, USA
A. van de Boer
Meteorology and Air Quality Section, Wageningen University, Wageningen, the Netherlands
O. Hartogensis
Meteorology and Air Quality Section, Wageningen University, Wageningen, the Netherlands
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- Lidar observations of atmospheric internal waves in the boundary layer of the atmosphere on the coast of Lake Baikal V. Banakh & I. Smalikho 10.5194/amt-9-5239-2016
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- Transition Periods in the Diurnally-Varying Atmospheric Boundary Layer Over Land W. Angevine et al. 10.1007/s10546-020-00515-y
- Mechanism of the effect of vertically propagating internal gravity waves on turbulence barrier and pollutant diffusion during heavy haze episodes Z. Wei et al. 10.1016/j.scitotenv.2022.157349
- Energy transition in the enhancement and break of turbulence barrier during heavy haze pollution Y. Ren et al. 10.1016/j.envpol.2022.120770
- The near‐surface evening transition L. Mahrt 10.1002/qj.3153
- Current Challenges in Orographic Flow Dynamics: Turbulent Exchange Due to Low-Level Gravity-Wave Processes S. Vosper et al. 10.3390/atmos9090361
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- Long-lived high-frequency gravity waves in the atmospheric boundary layer: observations and simulations M. Jia et al. 10.5194/acp-19-15431-2019
- Influence of Quasi-Periodic Oscillation of Atmospheric Variables on Radiation Fog over A Mountainous Region of Korea I. La et al. 10.3390/atmos11030230
- A study of local turbulence and anisotropy during the afternoon and evening transition with an unmanned aerial system and mesoscale simulation A. Lampert et al. 10.5194/acp-16-8009-2016
- Comparing mountain breezes and their impacts on CO2 mixing ratios at three contrasting areas C. Román-Cascón et al. 10.1016/j.atmosres.2019.01.019
- A Case Study of the Mechanisms Modulating the Evolution of Valley Fog C. Hang et al. 10.1007/s00024-016-1370-4
- A Case Study of Turbulence in the Nocturnal Boundary Layer During the Indian Summer Monsoon P. Deb Burman et al. 10.1007/s10546-018-0364-4
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- High-Resolution Observations of Transport and Exchange Processes in Mountainous Terrain S. Emeis et al. 10.3390/atmos9120457
- From weak to intense downslope winds: origin, interaction with boundary-layer turbulence and impact on CO<sub>2</sub> variability J. Arrillaga et al. 10.5194/acp-19-4615-2019
3 citations as recorded by crossref.
- Pollutant vertical mixing in the nocturnal boundary layer enhanced by density currents and low-level jets: two representative case studies M. Udina et al. 10.1007/s10546-019-00483-y
- Turbulence kinetic energy budget during the afternoon transition – Part 1: Observed surface TKE budget and boundary layer description for 10 intensive observation period days E. Nilsson et al. 10.5194/acp-16-8849-2016
- Interactions among drainage flows, gravity waves and turbulence: a BLLAST case study C. Román-Cascón et al. 10.5194/acp-15-9031-2015
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Latest update: 23 Apr 2024
Short summary
Stable-boundary-layer processes have been analysed using BLLAST data. Shallow drainage flows were formed at some locations after the near calm stage of the late afternoon. This stage ended with the arrival of a deeper wind associated with the mountain-plain circulation. At the same time, gravity waves were detected with an array of microbarometers. The interaction of these processes with turbulence was studied through multi-resolution flux decomposition at different sites and heights.
Stable-boundary-layer processes have been analysed using BLLAST data. Shallow drainage flows...
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