Articles | Volume 25, issue 3
https://doi.org/10.5194/hess-25-1245-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/hess-25-1245-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Evaluation of the dual-polarization weather radar quantitative precipitation estimation using long-term datasets
Tanel Voormansik
CORRESPONDING AUTHOR
Institute of Physics, University of Tartu, Tartu, Estonia
Numerical Modeling Department, Estonian Environment Agency, Tallinn, Estonia
Roberto Cremonini
Regional Agency for Environmental Protection of Piemonte,
Department for Natural and Environmental Risks, Turin, Italy
Institute for Atmospheric and Earth System Research/Physics,
University of Helsinki, Helsinki, Finland
Piia Post
Institute for Atmospheric and Earth System Research/Physics,
University of Helsinki, Helsinki, Finland
Radar Science, Finnish Meteorological Institute, Helsinki, Finland
Dmitri Moisseev
Institute for Atmospheric and Earth System Research/Physics,
University of Helsinki, Helsinki, Finland
Radar Science, Finnish Meteorological Institute, Helsinki, Finland
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In natural clouds, ice-nucleating particles are expected to be rare above –10 °C. In the current paper, we found that the formation of ice columns is frequent in stratiform clouds and is associated with increased precipitation intensity and liquid water path. In single-layer shallow clouds, the production of ice columns was attributed to secondary ice production, despite the rime-splintering process not being expected to take place in such clouds.
Haoran Li, Alexei Korolev, and Dmitri Moisseev
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Julia Schneider, Kristina Höhler, Paavo Heikkilä, Jorma Keskinen, Barbara Bertozzi, Pia Bogert, Tobias Schorr, Nsikanabasi Silas Umo, Franziska Vogel, Zoé Brasseur, Yusheng Wu, Simo Hakala, Jonathan Duplissy, Dmitri Moisseev, Markku Kulmala, Michael P. Adams, Benjamin J. Murray, Kimmo Korhonen, Liqing Hao, Erik S. Thomson, Dimitri Castarède, Thomas Leisner, Tuukka Petäjä, and Ottmar Möhler
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Piia Post and Margit Aun
Adv. Sci. Res., 17, 219–225, https://doi.org/10.5194/asr-17-219-2020, https://doi.org/10.5194/asr-17-219-2020, 2020
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The satellite-based fractional cloud cover and cloud top height from CLARA-A2 data record has been used to analyse trends in the Baltic Sea region, 1982–2015. Cloud observations from the Tartu-Tõravere meteorological station were used as reference data for the same period. A downward trend in fractional cloud cover in March over the 1982–2015 period was found. For cloud top heights summer and spring regional averages showed opposite signs of the trend: for June positive and for March negative.
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Short summary
A long set of operational polarimetric weather radar rainfall accumulations from Estonia and Italy are generated and investigated. Results show that the combined product of specific differential phase and horizontal reflectivity yields the best results when compared to rain gauge measurements. The specific differential-phase-based product overestimates weak precipitation, and the horizontal-reflectivity-based product underestimates heavy rainfall in all analysed accumulation periods.
A long set of operational polarimetric weather radar rainfall accumulations from Estonia and...