EMS Annual Meeting Abstracts
Vol. 18, EMS2021-262, 2021
https://doi.org/10.5194/ems2021-262
EMS Annual Meeting 2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.

Observations of an elevated rotor and precipitation processes decoupled during a mountain wave event in the Eastern Pyrenees (Cerdanya-2017 Field Experiment) 

Mireia Udina1, Joan Bech1, Sergi Gonzalez2, Alexandre Paci3, Laura Trapero4, Josep Ramón Miró5, and Bernat Codina1
Mireia Udina et al.
  • 1Universitat de Barcelona, Applied physics - Meteorology., Barcelona, Spain (mudina@meteo.ub.edu)
  • 2DT Catalonia, AEMET, 08005 Barcelona, Spain
  • 3CNRM, UMR3589 METEO-FRANCE and CNRS, 31100 Toulouse, Franc
  • 4Snow and Mountain Research Center of Andorra (CENMA-IEA), Institut d'Estudis, Andorrans, Av. Rocafort, 21-23, Sant Julià de Lòria AD600, Andorra T
  • 5Department of Territory and Sustainability, Meteorological Service of Catalonia, Generalitat de Catalunya, Barcelona, Spain

The study documents the formation of a rotor underneath the mountain waves generated the 15 January 2017 over the eastern Pyrenees (near the border between France, Spain and Andorra) during the Cerdanya-2017 field campaign. The event was characterized by strong winds, mountain waves and relevant snow accumulation over the Cerdanya valley and the eastern Pyrenees. The evolution and location of the mountain waves and precipitation structure were studied using high temporal resolution data from a UHF wind-profiler and a vertically pointing K-band Doppler radar, separated a few kilometres in horizontal distance.

A mountain wave was detected in the morning and shortened slightly in the afternoon when a transient rotor was formed disconnected from the surface flow (Udina et al. 2020). A strong turbulence zone was identified at the upper edge of the mountain wave, above the rotor, a feature observed in previous studies. The mountain wave and rotor induced circulation was favoured by the valley shape and the second mountain ridge location, in addition to the weak and variable winds, established during the sunset close to the valley surface. In addition, we find decoupling between precipitation processes and mountain wave induced circulations. During the studied event, mountain wave wind circulations and low-level turbulence do not affect neither the snow crystal riming or aggregation along the vertical column nor the surface particle size distribution of the snow. This study illustrates that precipitation profiles and mountain induced circulations may be decoupled which can be very relevant for either ground-based or spaceborne remote sensing of precipitation (Gonzalez et al 2019). This research is supported by CGL2015-65627-C3-1-R, CGL2015- 65627-C3-2-R (MINECO/FEDER), CGL2016-81828-REDT and RTI2018- 098693-B-C32 (AEI/FEDER).

References:

Gonzalez, S., Bech, J., Udina, M., Codina, B., Paci, A., & Trapero, L. (2019). Decoupling between precipitation processes and mountain wave induced circulations observed with a vertically pointing K-band doppler radar. Remote Sensing11(9), 1034.

Udina, M., Bech, J., Gonzalez, S., Soler, M. R., Paci, A., Miró, J. R., Trapero, L., Donier, J.M., Douffet, T., Codina, B., Pineda, N. (2020). Multi-sensor observations of an elevated rotor during a mountain wave event in the Eastern Pyrenees. Atmospheric Research234, 104698.

How to cite: Udina, M., Bech, J., Gonzalez, S., Paci, A., Trapero, L., Miró, J. R., and Codina, B.: Observations of an elevated rotor and precipitation processes decoupled during a mountain wave event in the Eastern Pyrenees (Cerdanya-2017 Field Experiment) , EMS Annual Meeting 2021, online, 6–10 Sep 2021, EMS2021-262, https://doi.org/10.5194/ems2021-262, 2021.

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