Abstract
This two‐part study presents a detailed analysis of (1) the vortex structure, (2) the inner‐core planetary boundary layer (PBL) wind profile, and (3) the overland surface winds of Typhoon Faxai (2019) during landfall observationally (Part I), and in high‐resolution Weather Research and Forecasting (WRF) model simulations (Part II). Part I presents a comprehensive observational analysis of (1), (2), and (3) of Typhoon Faxai (2019) based on radar dual‐Doppler analysis and spatially dense surface wind observations over the Kanto region of Japan. An empirical model for the wind reduction factor ( F 2 km ) is proposed and validated with surface observations and radar velocity‐azimuth display (VAD) analyses at Narita and Haneda airports, both of which were affected by the passage of Faxai's inner core. Two distinct PBL jets associated with the inner rainband and the eyewall were observed over Narita airport, which was located to the right of Faxai's track. Based on the empirical model of F 2 km , it is found that the maximum surface wind speed observed at Narita Airport was caused by the peak of F 2 km due to strong PBL jet associated with the eyewall located as close as ∼ 0.3 km from the ground. In addition, the wind swath analysis shows that a large area far inland on the right side of Faxai's track experienced strong surface 10‐minute winds due to the combination of the passage of the eyewall PBL jet and the small surface roughness length around agricultural land such as paddy fields and farm fields. This article is protected by copyright. All rights reserved.
