The Cross Equatorial Transport of the Hunga Tonga‐Hunga Ha'apai Eruption Plume

Author:

Schoeberl M. R.1ORCID,Wang Yi1ORCID,Ueyama R.2ORCID,Taha G.3ORCID,Yu W.4ORCID

Affiliation:

1. Science and Technology Corporation Columbia MD USA

2. NASA Ames Research Center Moffett Field CA USA

3. Morgan State University Baltimore MD USA

4. Hampton University Hampton VA USA

Abstract

AbstractOn 15 January 2022, the Hunga Tonga‐Hunga Ha'apai (HT) eruption injected SO2 and water into the middle stratosphere. Shortly after the eruption, the water vapor anomaly moved northward toward and across the equator. This northward movement appears to be due to equatorial Rossby waves forced by the excessive infrared water vapor cooling. Following the early eruption stage, persistent mid‐stratospheric water vapor and aerosol layers were mostly confined to Southern Hemisphere tropics (Eq. to 30°S). However, during the spring of 2022, the westerly phase of the tropical quasi‐biennial oscillation (QBO) descended through the tropics. The HT water vapor and aerosol anomalies were observed to again move across the equator coincident with the shift in the Brewer‐Dobson circulation and the descent of the QBO shear zone.

Funder

Earth Sciences Division

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

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