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Alpine planetary boundary layer information


PBL over a mountainous terrain (left hand side) vs. a flat terrain (right hand side)

The alpine planetary boundary layer is the planetary boundary layer (PBL) associated with mountainous regions. Due to its high spatial and temporal variability, its behavior is more complex than over a flat terrain. The fast changing local wind system directly linked to topography and the variable land cover that goes from snow to vegetation have a significant effect on the growth of the PBL and make it much harder to predict.

Understanding the processes inducing changes in the mountain PBL have critical applications for predicting air pollution transport,[1] fire weather and local intense thunderstorm events. While some processes, such as mountain waves, have been well studied in the mountain PBL due to their importance for aviation, most of the behaviors of the alpine PBL are relatively unknown.[2]

  1. ^ Henne, S.; Dommen, J.; Neiniger, B.; Reimann, S.; Staehelin, J.; Prévôt, A. (2005). "Influence of mountain venting in the Alps on the ozone chemistry of the lower free troposphere and the European pollution export". Journal of Geophysical Research. 110 (D22): D22307. Bibcode:2005JGRD..11022307H. doi:10.1029/2005jd005936.
  2. ^ Investigation of the Planetary Boundary Layer in the Swiss Alps Using Remote Sensing and In Situ Measurements

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