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https://meetingorganizer.copernicus.org/EGU24/EGU24-11374.html

*AUTHORS*
Clarissa Kroll and Robert Jnglin Wills

*How to cite:* Kroll, C. and Jnglin Wills, R.: The El Niño response to
tropical volcanic eruptions and geoengineering , EGU General Assembly 2024,
Vienna, Austria, 14–19 Apr 2024, EGU24-11374,
https://doi.org/10.5194/egusphere-egu24-11374, 2024.

*ABSTRACT*
Following tropical volcanic eruptions and in response to geoengineering
efforts in climate models, the occurrence of El Niño is notably enhanced.
However, the precise mechanisms leading to the preference of the El Niño
state remain a subject of ongoing debate. In this study, we explore the El
Niño response within the context of stratospheric aerosol injection
experiments using the Community Earth System Model version 1, with the
Whole Atmosphere Community Climate Model atmospheric component (CESM1
WACCM). Our investigation is centered around the Stratospheric Aerosol
Geoengineering Large Ensemble Dataset encompassing three distinct
scenarios: a simulation of the RCP8.5 scenario as baseline climate change
scenario, a geoengineering scenario, in which surface temperature increases
are completely compensated and a scenario focusing solely on the
stratospheric heating derived from the geoengineering approach. Our
analysis reveals that the El Niño response is primarily linked to the
heating in the tropical tropopause layer and lower stratosphere, and
notably, it occurs independently of tropospheric cooling effects. We
explain the increased occurrence of El Niño after volcanic eruptions and
simulated geoengineering interventions by a slow down of the tropical
atmospheric circulation, which is caused by increases in gross moist
stability due to aerosol heating in tropical tropopause layer.

*Source: EGU GENERAL ASSEMBLY 2024*

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