https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2022MS003532

*Authors*
Chloe Yuchao Gao
<https://agupubs.onlinelibrary.wiley.com/authored-by/ContribAuthorRaw/Gao/Chloe+Yuchao>
, Vaishali Naik
<https://agupubs.onlinelibrary.wiley.com/authored-by/ContribAuthorRaw/Naik/Vaishali>
, Larry W. Horowitz
<https://agupubs.onlinelibrary.wiley.com/authored-by/ContribAuthorRaw/Horowitz/Larry+W.>
, Paul Ginoux
<https://agupubs.onlinelibrary.wiley.com/authored-by/ContribAuthorRaw/Ginoux/Paul>
, Fabien Paulot
<https://agupubs.onlinelibrary.wiley.com/authored-by/ContribAuthorRaw/Paulot/Fabien>
, John Dunne
<https://agupubs.onlinelibrary.wiley.com/authored-by/ContribAuthorRaw/Dunne/John>
, Michael Mills
<https://agupubs.onlinelibrary.wiley.com/authored-by/ContribAuthorRaw/Mills/Michael>
, Valentina Aquila
<https://agupubs.onlinelibrary.wiley.com/authored-by/ContribAuthorRaw/Aquila/Valentina>
, Peter Colarco
<https://agupubs.onlinelibrary.wiley.com/authored-by/ContribAuthorRaw/Colarco/Peter>
First published: *20 May 2023*
https://doi.org/10.1029/2022MS003532


Abstract

Stratospheric injections of sulfur dioxide from major volcanic eruptions
perturb the Earth's global radiative balance and dominate variability in
stratospheric sulfur loading. The atmospheric component of the GFDL Earth
System Model (ESM4.1) uses a bulk aerosol scheme and previously prescribed
the distribution of aerosol optical properties in the stratosphere. To
quantify volcanic contributions to the stratospheric sulfur cycle and the
resulting climate impact, we modified ESM4.1 to simulate stratospheric
sulfate aerosols prognostically. Driven by explicit volcanic emissions of
aerosol precursors and non-volcanic sources, we conduct ESM4.1 simulations
from 1989 to 2014, with a focus on the Mt. Pinatubo eruption. We evaluate
our interactive representation of the stratospheric sulfur cycle against
data from Moderate Resolution Imaging Spectroradiometer, Multi-angle
Imaging SpectroRadiometer, Advanced Very High Resolution Radiometer, High
Resolution Infrared Radiation Sounder, and Stratospheric Aerosol and Gas
Experiment II. To assess the key processes associated with volcanic
aerosols, we performed a sensitivity analysis of sulfate burden from the
Mt. Pinatubo eruption by varying injection heights, emission amount, and
stratospheric sulfate's dry effective radius. We find that the simulated
stratospheric sulfate mass burden and aerosol optical depth in the model
are sensitive to these parameters, especially volcanic SO2 injection
height, and the optimal combination of parameters depends on the metric we
evaluate.
Key Points


   -

   We present an interactive representation of the stratospheric sulfur
   cycle in GFDL ESM4 that replaced prescribed aerosol optical properties
   -

   We simulated years 1989–2014 with a focus on the Mt. Pinatubo eruption
   and evaluated against observations
   -

   Simulated stratospheric sulfate burden and optical depth are sensitive
   to injection height, emission amount, and aerosol size

Plain Language Summary

Major volcanic eruptions emit sulfur dioxide into the stratosphere and
affect the Earth's global radiative balance as well as the stratospheric
sulfur abundance. The GFDL Earth System Model (ESM4.1) previously uses
prescribed aerosol optical properties, and in this paper, we replace it
with explicit volcanic emissions to study the volcanic contribution to the
stratospheric sulfur cycle and its impact. We simulate years from 1989 to
2014, with a focus on the Mt. Pinatubo eruption as a benchmark. We also
evaluate the new improvements against observations and performed
sensitivity analyses of the sulfate burden from the Mt. Pinatubo eruptions.
We find that the simulated stratospheric sulfate amount and aerosol optical
depth are sensitive to injection height, emission amount, and aerosol size,
and while the injection height is the most sensitive, the best combination
of parameters depends on the chosen observational metric.


*Source: AGU*

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