Microphysical Simulation of the 2022 Hunga Volcano Eruption Using a Sectional Aerosol Model
Chenwei Li, Yifeng Peng, Elizabeth Asher, Alexandre Baron, Michael A. Todt, Troy Thornberry, Stéphanie Evan, J. Brioude, Penny Smale, Richard Querel, Karen H. Rosenlof, Luxi Zhou, Jingyuan Xu, Kai Qie, Jianchun Bian, O. B. Toon, Yunqian Zhu, Pengfei Yu
Abstract
Abstract Approximately 150 Tg of water vapor and 0.42 Tg of sulfur dioxide were injected directly into the stratosphere by the January 2022 Hunga volcanic eruption, which represents the largest water vapor injection in the satellite era. A comparison of numerical simulations to balloon‐borne and satellite observations of the water‐rich plume suggests that particle coagulation contributed to the Hunga aerosol's effective dry radius increase from 0.2 μm in February to around 0.4 μm in March. Our model suggests that the stratospheric aerosol effective radius is persistently perturbed for years by moderate and large‐magnitude volcanic events, whereas extreme wildfire events show limited impact on the stratospheric background particle size. Our analysis further suggests that both the particle optical efficiency and the aerosols' stratospheric lifetime explain Hunga's unusually large aerosol optical depth per unit of the SO 2 injection, as compared with the Pinatubo eruption.