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The Estimated Climate Impact of the Hunga Tonga‐Hunga Ha'apai Eruption Plume

2023; American Geophysical Union; Volume: 50; Issue: 18 Linguagem: Inglês

10.1029/2023gl104634

1944-8007

M. R. Schoeberl, Yi Wang, Rei Ueyama, A. E. Dessler, Ghassan Taha, Wandi Yu,

Atmospheric and Environmental Gas Dynamics

Abstract On 15 January 2022, the Hunga Tonga‐Hunga Ha'apai (HT) eruption injected SO 2 and water into the middle stratosphere. The SO 2 is rapidly converted to sulfate aerosols. The aerosol and water vapor anomalies have persisted in the Southern Hemisphere throughout 2022. The water vapor anomaly increases the net downward IR radiative flux whereas the aerosol layer reduces the direct solar forcing. The direct solar flux reduction is larger than the increased IR flux. Thus, the net tropospheric forcing will be negative. The changes in radiative forcing peak in July and August and diminish thereafter. Scaling to the observed cooling after the 1991 Pinatubo eruption, HT would cool the 2022 Southern Hemisphere's average surface temperatures by less than 0.037°C.