Preprints
https://doi.org/10.5194/egusphere-2024-430
https://doi.org/10.5194/egusphere-2024-430
12 Mar 2024
 | 12 Mar 2024
Status: this preprint is open for discussion and under review for Atmospheric Chemistry and Physics (ACP).

Observed and CMIP6 model simulated organic aerosol response to drought in the contiguous United States during summertime

Wei Li and Yuxuan Wang

Abstract. Drought events have been linked with the enhancements of organic aerosols (OA), but the mechanisms have not been comprehensively understood. This study investigates the relationships between the monthly standardized precipitation–evapotranspiration index (SPEI) and surface OA in the contiguous United States (CONUS) during the summertime from 1998 to 2019. OA under severe drought conditions shows a significant increase in mass concentrations across most of the CONUS relative to non-drought periods with the Pacific Northwest (PNW) and Southeastern United States (SEUS) experiencing the highest average enhancement of 1.79 µg m−3 (112 %) and 0.92 µg m−3 (33 %), respectively. In the SEUS, a linear regression approach between OA and sulfate was used to estimate the isoprene epoxydiols derived secondary organic aerosol (IEPOX SOA), which is the primary driver of the OA enhancements under droughts due to the simultaneous increase of isoprene and sulfate. The rise of sulfate is mainly caused by the reduced wet deposition because of the up to 62 % lower precipitation amount. In the PNW, OA enhancements are closely linked to intensified wildfire emissions, which raise OA mass concentrations to be four to eight times higher relative to non-fire conditions. All ten Earth system models participating in the sixth phase of the Coupled Model Intercomparison Project (CMIP6) can capture the negative slopes between SPEI and OA in the PNW with CESM2-WACCM and GFDL-ESM4 performing the best and worst in predicting the OA enhancement under severe droughts. However, all models significantly underestimate the OA increase in the SEUS with Nor-ESM2-LM and MIRCO6 showing relatively better performance. This study reveals the key drivers of the elevated OA levels under droughts in the CONUS and underscores the deficiencies of current climate models in their predictive capacity for assessing the impact of future droughts on air quality.

Wei Li and Yuxuan Wang

Status: open (until 23 Apr 2024)

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Wei Li and Yuxuan Wang
Wei Li and Yuxuan Wang

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Short summary
This study finds that droughts immensely increased organic aerosol (OA) in the contiguous U.S. during summertime 1998–2019, notably in the Pacific Northwest (PNW) and Southeast (SEUS). The rise of OA in the SEUS is mainly driven by the enhanced formation of isoprene epoxydiols derived secondary organic aerosol due to the increase of isoprene and sulfate, while in the PNW, it is caused by wildfires. Ten climate models captured the OA increase in the PNW, yet greatly underestimated it in the SEUS.