I. Introduction
Passive microwave remote sensing can obtain atmospheric parameters inside clouds and precipitation, playing a crucial role in weather forecasting [1]. The existing microwave atmospheric sounders are, however, equipped with a limited number of polar-orbiting meteorological satellites, restricting the ability to collect high-frequency temporal observations for specific regions [2]. Although geostationary satellites have the unique advantage of continuously monitoring the Earth in meteorological applications, achieving high spatial resolution geostationary microwave observations still faces technical challenges.