I. Introduction
Weather radars are very useful for estimating rainfall amounts because they can measure instantaneous rain rates and their distribution at fine spatial and temporal resolutions compared with rain gauges [1]. Typical operating temporal and spatial resolutions of weather radars are 1–5 min and 100 m–1 km for the X-band, 5–10 min and 250 m–2 km for the C-band, 10–15 min and 1–4 km for the S-band, respectively [2].