Synergy of GPM and ground-based radar observations for precipitation estimation and detection of microphysical processes

• Published in: 2018 19th International Radar Symposium (IRS) pp. 1 - 8
• Main Authors: Pejcic, Velibor, Tromel, Silke, Muhlbauer, Kai, Saavedra, Pablo, Beer, Josephin, Simmer, Clemens
• Format: Conference Proceeding
• Language: English
• Published: German Institute of Navigation - DGON 01.06.2018
• Subjects: Correlation; Meteorological radar; Radar polarimetry; Reflectivity; Satellites; Spaceborne radar
• ISSN: 2155-5753
• DOI: 10.23919/IRS.2018.8447923

The Global Precipitation Measurement core satellite (GPM) operates with a Ku-band and Ka-band Dual-frequency Precipitation Radar (DPR). This first space-borne DPR allows important global insights into three-dimensional precipitation structures from space. The polarimetric X-band research radar in Bonn (BoXPol), Germany, is part of an international network for ground validation of the GPM satellite. The nationwide German C-band radar network of the German Weather Service (RADOLAN) and a vertically pointing Micro Rain Radar (MRR) are used to evaluate the satellite based precipitation estimates, rain type and phase partitioning (solid, liquid, mixed phase). Three years of comparison (2014-2017) between GPM DPR and the ground-based observations from RADOLAN and BoXPol show high correlations. The near surface rain rates and reflectivities from the single and dual-frequency satellite products reveal robust correlations in summer but higher variability in winter. This can be attributed to reduced DPR performance for solid precipitation estimates which directly depends on the melting layer detection. Therefore, GPM-based vertical products like the bright band height and thickness used for phase partitioning require an in-depth evaluation. The measurements of the polarimetric X-band radars in Bonn and Jülich allow a more reliable and robust detection of the bright band which is compared with GPM-based results. The use of the temporal evolution of quasi vertical profiles (QVP) and column vertical profiles (CVP) sustain the polarimetric information and offer an optimal detection of the melting layer and phase partitioning during the development of precipitation systems. Furthermore, contoured frequency by altitude diagrams (CFAD) are used to compare reflectivity distributions.