Articles | Volume 14, issue 23
https://doi.org/10.5194/acp-14-13205-2014
© Author(s) 2014. 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-14-13205-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Determination and climatology of the planetary boundary layer height above the Swiss plateau by in situ and remote sensing measurements as well as by the COSMO-2 model
M. Collaud Coen
Federal Office of Meteorology and Climatology, MeteoSwiss, 1530 Payerne/8044 Zurich, Switzerland
C. Praz
now at: ESA Advanced Concept Team, ESTEC, Keplerlaan 1, 2201 AZ Noordwijk, the Netherlands
Federal Office of Meteorology and Climatology, MeteoSwiss, 1530 Payerne/8044 Zurich, Switzerland
A. Haefele
Federal Office of Meteorology and Climatology, MeteoSwiss, 1530 Payerne/8044 Zurich, Switzerland
D. Ruffieux
Federal Office of Meteorology and Climatology, MeteoSwiss, 1530 Payerne/8044 Zurich, Switzerland
P. Kaufmann
Federal Office of Meteorology and Climatology, MeteoSwiss, 1530 Payerne/8044 Zurich, Switzerland
B. Calpini
Federal Office of Meteorology and Climatology, MeteoSwiss, 1530 Payerne/8044 Zurich, Switzerland
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Short summary
An operational planetary boundary layer height detection method with several remote sensing instruments (wind profiler, Raman lidar, microwave radiometer) and algorithms (Parcel and bulk Richardson number methods, surface-based temperature inversion, aerosol and humidity gradient analysis) was validated against radio sounding. A comparison with the numerical weather prediction model COSMO-2 and the seasonal cycles of the day- and nighttime PBL for two stations on the Swiss plateau are presented.
An operational planetary boundary layer height detection method with several remote sensing...
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