Articles | Volume 14, issue 1
https://doi.org/10.5194/amt-14-511-2021
© 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/amt-14-511-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Linking rain into ice microphysics across the melting layer in stratiform rain: a closure study
National Centre for Earth Observation, University of Leicester, Leicester, UK
Alessandro Battaglia
Earth Observation Science, Department of Physics and Astronomy, University of Leicester, Leicester, UK
Department of Environmental, Land and Infrastructure Engineering (DIATI), Politecnico of Turin, Turin, Italy
Stefan Kneifel
Institute for Geophysics and Meteorology, University of Cologne, Cologne, Germany
Leonie von Terzi
Institute for Geophysics and Meteorology, University of Cologne, Cologne, Germany
Markus Karrer
Institute for Geophysics and Meteorology, University of Cologne, Cologne, Germany
Davide Ori
Institute for Geophysics and Meteorology, University of Cologne, Cologne, Germany
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- Validation of Synthetic Storm Technique for Rain Attenuation Prediction Over High-Rainfall Tropical Region S. Chakraborty et al. 10.1109/LGRS.2021.3068334
- Advantages of G-band radar in multi-frequency liquid-phase microphysical retrievals B. Courtier et al. 10.5194/amt-17-6875-2024
- First Observations of G‐Band Radar Doppler Spectra B. Courtier et al. 10.1029/2021GL096475
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- Triple-frequency radar retrieval of microphysical properties of snow K. Mroz et al. 10.5194/amt-14-7243-2021
- Enhancing consistency of microphysical properties of precipitation across the melting layer in dual-frequency precipitation radar data K. Mroz et al. 10.5194/amt-17-1577-2024
- Direct Comparisons between GPM-DPR and CloudSat Snowfall Retrievals R. Chase et al. 10.1175/JAMC-D-21-0081.1
2 citations as recorded by crossref.
Latest update: 13 Dec 2024
Short summary
The article examines the relationship between the characteristics of rain and the properties of the ice cloud from which the rain originated. Our results confirm the widely accepted assumption that the mass flux through the melting zone is well preserved with an exception of extreme aggregation and riming conditions. Moreover, it is shown that the mean (mass-weighted) size of particles above and below the melting zone is strongly linked, with the former being on average larger.
The article examines the relationship between the characteristics of rain and the properties of...