Influence of the transported Canadian wildfire smoke on the ozone and particle pollution over the Mid-Atlantic United States

Date

2022-01-14

Department

Program

Citation of Original Publication

"Yang, Zhifeng et al. Influence of the transported Canadian wildfire smoke on the ozone and particle pollution over the Mid-Atlantic United States. Atmospheric Environment 273 (15 March 2022) 118940. https://doi.org/10.1016/j.atmosenv.2022.118940"

Rights

This work was written as part of one of the author's official duties as an Employee of the United States Government and is therefore a work of the United States Government. In accordance with 17 U.S.C. 105, no copyright protection is available for such works under U.S. Law.
Public Domain Mark 1.0

Subjects

Abstract

The integration of observations and models can improve air quality forecasts (in particular ozone (O₃) and particulate matter (PM)) for extreme events (e.g., wildfires). We present our work on the Canadian wildfire event on 6–12 June 2015 that impacted the air quality in the Mid-Atlantic region in the U.S. We use the Weather Research and Forecasting model coupled with Chemistry package (WRF-Chem), and various measurements from both ground-based and spaceborne observations, including the U.S. Environmental Protection Agency (EPA) AirNow data, the National Aeronautics and Space Administration (NASA) operated TROPospheric OZone lidar (TROPOZ), wind radar profiler, ceilometer, Moderate Resolution Imaging Spectroradiometer (MODIS), Cloud- Aerosol Lidar with Orthogonal Polarization (CALIOP). The objective is to understand the physics of the Plane- tary Boundary Layer (PBL) and its role on the O₃ and PM forecast. The findings show that the model captured the O₃ diurnal variation and PM spatial distribution both horizontally and vertically by comparing with EPA AirNow and MODIS/CALIOP observations, respectively. Wildfire smoke was transported from central Canada through Lake Michigan, passing the Ohio River Valley and down to the Baltimore-Washington D.C. metropolis. The night- time O₃ mixing ratio reached 30 ppbv, while the daytime O₃ mixing ratio approached larger than 100 ppbv near AirNow stations in Maryland, due to the mixing of the transported smoke into the PBL. The novel NASA TROPOZ lidar at Beltsville resolved the O₃ vertical profile and the ceilometer identified the smoke intrusion at altitudes above 3.5 km, but later mixed down into the PBL and surface which was also resolved by the model. Thus, integrating both model and observations from different platforms confirms the Canadian wildfire source and transport pathway and improves the understanding of the air quality forecast during the extreme wildfire event.