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High ozone (O 3 ) episodes frequently occur in New York metropolitan and the downwind coastal area in summer. In this study, lidar/ceilometer are combined with WRF/Chem model to investigate an O 3  event on Aug. 27~30 2018. We examine the spatial-temporal variabilities of O 3  and planetary-boundary-layer height (PBLH) and assess the model performance on simulating surface O 3  during this episode. By comparing with the lidar observations, the WRF/Chem is able to capture high O 3  distribution in the PBL at noon and indicates consistent diurnal evolution for the ground O 3 . Nevertheless, in the early morning and night, the model overestimates the ground O 3  and underestimates the PBLH.

Variation of Ozone and PBL from the Lidar Observations and WRF-Chem Model in NYC Area During the 2018 Summer LISTOS Campaign