The original WLRAS uses a triply nested domain with the finest horizontal resolution of 4 km, and the assimilation frequency is 15 minutes. Experimental results show that increasing the model horizontal resolution from 4 km to 1.33 km at the forecast stage can alleviate the spindown issue. Furthermore, the spindown is better resolved when the model resolution is increased earlier at the DA stage. Such results indicate that the high-resolution model is important not only for the forecast but also for the analysis performance. The positive impact of increasing model resolution is attributed to the better-resolved secondary circulation at the eyewall and the stronger warm core structure. Experimental results also show that using either 15-, 30-, and 60-minute assimilation intervals can establish good tangential wind structure within 3 hours, but only the 15-minute rapid update cycle is able to reconstruct the complete typhoon circulation and sustains typhoon intensity after a 12-hour forecast. It reveals that the rapid update cycle is critical for assimilating the dense radar data to obtain an accurate TC analysis and forecast.

