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Pollen forecasts in complex topography: two case studies from the Alps using the numerical pollen forecast model COSMO-ART

  • Andreas PaulingEmail author
  • Bernard Clot
  • Annette Menzel
  • Stephan Jung
Original Paper
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Abstract

Pollen concentrations on Alpine mountain tops are poorly known due to few observations and few modeling studies. We present two case studies from the Alps that provide insights into the spatial and temporal distribution of birch pollen. The numerical pollen dispersion model COSMO-ART (COnsortium for Small-scale MOdelling-Aerosols and Reactive Trace gases) was used to simulate the birch pollen transport during the 2017 pollen season. The model configuration included 1.1-km horizontal grid spacing and 80 vertical levels. The simulations were compared with daily pollen concentrations from two mountain tops in the Alps (Weissfluhjoch near Davos, Switzerland, at 2692 m and Schneefernerhaus, Germany, at 2650 m a.s.l.). In addition, the Swiss pollen stations at Davos (1587 m a.s.l.) and Buchs (446 m a.s.l.) were used. COSMO-ART simulations agreed well with the observations at Davos and Weissfluhjoch. At the Environmental Research Station Schneefernerhaus, the pollen concentrations were generally overestimated. We analyzed the pollen transport episode of 9 April 2017 at Weissfluhjoch in more detail using vertical cross sections of the COSMO-ART simulations. The results suggest that pollen can be lifted up to 3000 m in the morning hours and are subsequently transported by large-scale winds leading to higher birch pollen concentrations at Weissfluhjoch than at Davos. This suggests that the actual situation regarding sources, topography and wind determines the pollen distribution and not only altitude. Still, pollen levels at Weissfluhjoch are more than one order of magnitude lower than typical pollen levels at lowland Swiss stations such as Buchs.

Keywords

High-resolution pollen forecasts COSMO-ART Complex topography Birch pollen Pollen dispersion models Pollen transport 

Notes

Acknowledgements

We thank the team of the Institute for Snow and Avalanche Research in Davos and the team of the Environmental Research Station Schneefernerhaus for their accurate service w.r.t. to the pollen traps. Likewise, we are grateful to Guy de Morsier from MeteoSwiss for his help in preparing Figs. 1 and 3. This study was also supported by the Swiss National Supercomputing Centre (CSCS) under project ID s83.

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Copyright information

© Springer Nature B.V. 2019

Authors and Affiliations

  1. 1.Federal Office of Meteorology and Climatology MeteoSwissZurich-AirportSwitzerland
  2. 2.Federal Office of Meteorology and Climatology MeteoSwissPayerneSwitzerland
  3. 3.Ecoclimatology, TUM School of Life SciencesTechnical University of MunichFreisingGermany

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