[HTML][HTML] Retrievals of ice microphysical properties using dual-wavelength polarimetric radar observations during stratiform precipitation events

E Tetoni, F Ewald, M Hagen, G Köcher… - Atmospheric …, 2022 - amt.copernicus.org
Ice growth processes within clouds affect the type and amount of precipitation. Hence, the
importance of an accurate representation of ice microphysics in numerical weather and …

Retrieval of the raindrop size distribution from polarimetric radar data using double-moment normalisation

TH Raupach, A Berne - Atmospheric Measurement Techniques, 2017 - amt.copernicus.org
A new technique for estimating the raindrop size distribution (DSD) from polarimetric radar
data is proposed. Two statistical moments of the DSD are estimated from polarimetric …

From model to radar variables: a new forward polarimetric radar operator for COSMO

D Wolfensberger, A Berne - Atmospheric Measurement …, 2018 - amt.copernicus.org
In this work, a new forward polarimetric radar operator for the COSMO numerical weather
prediction (NWP) model is proposed. This operator is able to simulate measurements of …

[HTML][HTML] Unsupervised classification of vertical profiles of dual polarization radar variables

J Tiira, D Moisseev - Atmospheric Measurement Techniques, 2020 - amt.copernicus.org
Vertical profiles of polarimetric radar variables can be used to identify fingerprints of snow
growth processes. In order to systematically study such manifestations of precipitation …

Detection of the melting level with polarimetric weather radar

D Sanchez-Rivas… - Atmospheric Measurement …, 2021 - amt.copernicus.org
Accurate estimation of the melting level (ML) is essential in radar rainfall estimation to
mitigate the bright band enhancement, classify hydrometeors, correct for rain attenuation …

Characterisation of the melting layer variability in an Alpine valley based on polarimetric X-band radar scans

F van den Heuvel, M Gabella… - Atmospheric …, 2018 - amt.copernicus.org
The melting layer designates the transition region from solid to liquid precipitation, and is a
typical feature of the vertical structure of stratiform precipitation. As it is characterised by a …