The module for assimilating radiance data of the Microwave Humidity Sounder-2 (MWHS-2) onboard the Feng Yun 3D (FY-3D) satellite is built in the Weather Research and Forecasting (WRF) model data assimilation (WRFDA) system. The CONV, 3DVar, and EnVar experiments are conducted to investigate the impact of assimilating the new humidity sounder based on Typhoon Ampil (2018). Both the 3DVar and EnVar experiments assimilate FY-3D MWHS-2 radiance data on top of the conventional data, while the CONV experiment only applies conventional data. In the EnVar experiment, notable geopotential height increment is observed around the typhoon, leading the typhoon to move northeast. In addition, the moisture field is improved to some extent. Finally, from the analysis of the dynamic field of the typhoon, it can be found that the EnVar experiment can adjust the dynamic structure of the typhoon. Furthermore, the assimilation of FY-3D MWHS-2 radiance data reduces the forecast error of the typhoon track and intensity. Additionally, the precipitation skill is improved in terms of rainfall pattern and the verification score. This improvement in the precipitation may be closely related to the features of the circulation structure concerning the evolution of the typhoon. The improved prediction of the position and intensity of rainbands in the FY-3D MWHS-2 radiance data assimilation experiment corresponds to a better prediction of typhoon structure.

Geostationary infrared observations provide frequent, spatially continuous information on rapidly evolving convective systems. This study assimilates clear-sky and all-sky Channel 10 brightness temperatures (BTs) from GOES-R Advanced Baseline Imager (ABI). The impacts on the analysis and short-range forecast of a continental meso-scale convective system (MCS) are compared. The implementation is achieved in a convection-permitting model using a 5 min cycling ensemble Kalman filter (EnKF) framework. A quality control procedure is developed to enable the effective assimilation of clear-sky ABI observations. Results show that clear-sky assimilation partially removes spurious background clouds and adjusts temperature and moisture in the near-storm environment. All-sky assimilation substantially improves the analyzed cloud field, produces stronger in-storm thermodynamic and dynamical increments, as well as directly constrains hydrometeor variables. In addition, assimilating all-sky observations reduces errors of analyzed surface temperature and humidity by over 25%. Forecast verification further indicates that all-sky assimilation provides more persistent forecast improvements in terms of BT and reflectivity quantities than clear-sky assimilation does. Both clear-sky and all-sky assimilations improve the spatial coverage and intensity of accumulated precipitation, but assimilating all-sky observations produces substantially larger FSS gains (0.163–0.380 versus 0.02–0.13).

In previous studies, radar reflectivity is often directly assimilated using reflectivity operators based on a single-moment (SM) microphysics scheme, though the forecast model uses a double-moment (DM) microphysics scheme. With the fixed number concentrations, only the mixing ratios of hydrometeors are directly updated during the assimilation, which leads to a mismatch between the analyzed microphysical state variables and the microphysics scheme of the forecast model. In this study, the radar reflectivity is directly assimilated through an observation operator consistent with the DM Thompson microphysics scheme used in numerical integrations, and the impact of reflectivity operators based on SM and DM schemes on the analysis performance of the ensemble Kalman filter for typhoon Lekima on 9 August 2019 is evaluated. Reflectivity observations from a single operational weather radar in Wenzhou City, Zhejiang Province of China are assimilated. In addition, the dual-polarization observations from the same radar are used to evaluate the quality of the analysis. The analyzed reflectivity and dual-polarization characteristics obtained by different reflectivity operators are examined in detail. Compared with the experiments applying the reflectivity operator based on the SM Lin scheme, the use of a reflectivity operator consistent with the DM Thompson scheme adopted in the forecast model results in analyzed reflectivity and polarization characteristics that are more consistent with the observed characteristics in terms of general structure, location, and intensity. Forecasted reflectivity, 3 h accumulated precipitation, and typhoon intensity and track are also evaluated. The application of the reflectivity operator based on the DM scheme makes better forecasts of typhoon intensity, precipitation, and reflectivity, which also improves the forecast skills on typhoon tracks to a certain extent.