Observation of the Aerosol Plume From the 2022 Hunga Tonga—Hunga Ha'apai Eruption With SAGE III/ISS

Author:

Duchamp Clair1ORCID,Wrana Felix2ORCID,Legras Bernard1ORCID,Sellitto Pasquale34ORCID,Belhadji Redha3ORCID,von Savigny Christian2ORCID

Affiliation:

1. Laboratoire de Météorologie Dynamique (LMD‐IPSL) CNRS Sorbonne Université ENS‐PSL École Polytechnique Paris France

2. Institute of Physics University of Greifswald Greifswald Germany

3. Université Paris Est Créteil Université de Paris‐Cité CNRS Laboratoire Interuniversitaire des Systèmes Atmosphériques (LISA‐IPSL) Créteil France

4. Istituto Nazionale di Geofisica e Vulcanologia (INGV) Osservatorio Etneo (OE) Catania Italy

Abstract

AbstractThe Tonga eruption of 15 January 2022 has released a long‐lived stratospheric plume of sulfate aerosols. More than 17 months after, we focus on the high quality data series of SAGE III (Stratospheric Aerosol and Gas Experiment) on board the International Space Station (ISS) to determine the mean radius and size distribution of the aerosols and their total mass. The persisting volcanic aerosols—with a mode width of 1.25 and an effective radius of 0.4 μm—differ from the significantly smaller background aerosols and from those measured during recent stratospheric eruptions. The sulfuric acid mass between 50°S and 30°N is estimated to be very stable in spite of considerable redistribution in latitude at a value of 0.66 ± 0.1 Tg, corresponding to an initial sulfur dioxide emission of 0.44 Tg. Such properties are expected to facilitate the persistence of a climate warming due to the volcanic water vapor.

Funder

Agence Nationale de la Recherche

Centre National d’Etudes Spatiales

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

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