Japan Geoscience Union Meeting 2025

Presentation information

[E] Oral

A (Atmospheric and Hydrospheric Sciences ) » A-AS Atmospheric Sciences, Meteorology & Atmospheric Environment

[A-AS07] The Beginning of Cloud Aerosol and Radiation Sciences with EarthCARE

Fri. May 30, 2025 10:45 AM - 12:15 PM Exhibition Hall Special Setting (5) (Exhibition Hall 7&8, Makuhari Messe)

convener:Takuji Kubota(Earth Observation Research Center,Japan Aerospace Exploration Agency), Hajime Okamoto(Kyushu University), Masaki Satoh(Atmosphere and Ocean Research Institute, The University of Tokyo), Nobuhiro Takahashi(Institute for Space-Earth Environmental Research, Nagoya University), Chairperson:Nobuhiro Takahashi(Institute for Space-Earth Environmental Research, Nagoya University), Takuji Kubota(Earth Observation Research Center,Japan Aerospace Exploration Agency)


12:00 PM - 12:15 PM

[AAS07-12] Preliminary evaluation of EarthCARE/CPR for the global data assimilation

★Invited Papers

*Kozo OKAMOTO1, Izumi Okabe1, Gennosuke Kikuchi2, Toshiyuki Tanaka3, Takuji Kubota3 (1.Meteorological Research Institute, 2.RESTEC, 3.JAXA)

Keywords:data assimilation, CPR, global numerical weather prediction, satellite

The space-based cloud profiling radar (CPR) is valuable in evaluating and improving cloud processes of numerical weather prediction (NWP) and climate models. Assimilating CPR will also be beneficial for improving accuracy in NWP analysis and forecasts. Successful assimilation of CPR observations requires a deep understanding of the characteristics of CPR observation and its simulation from NWP model used in the data assimilation system. This study aims to evaluate simulation by comparing CPR observation and simulation made by the global model at Japan Meteorological Agency.

This comparison study started for CloudSat/CPR and now deals with EarthCARE/CPR. RTTOV ver13.0 is used as a radar simulator to simulate assimilation variables of radar reflectivity. EarthCARE/CPR reflectivity observations are obtained from L2a CPR One-sensor Echo Product and averaged to match an assimilation horizontal scale (~55 km). The comparison for three weeks in August 2024 shows that simulated reflectivity is smaller in its variability and slightly weaker in mean echo than observed reflectivity except at high altitudes. The reflectivity departure of observation from the simulation is carefully examined because it is especially important for data assimilation. For example, its probability density function, situation dependency, and scale representativity are being examined. In the meeting, we will present the latest findings and discuss how to effectively assimilate EarthCARE/CPR.