https://agupubs.onlinelibrary.wiley.com/doi/abs/10.1029/2020JD033438

Aerosol Dynamics in the Near Field of the SCoPEx Stratospheric Balloon
Experiment
C. M. Golja L. W. Chew J. A. Dykema D. W. Keith
First published: 01 February 2021
https://doi.org/10.1029/2020JD033438

Abstract
Stratospheric aerosol injection (SAI) might alleviate some climate risks
associated with accumulating greenhouse gases. Reduction of specific
process uncertainties relevant to the distribution of aerosol in a
turbulent stratospheric wake is necessary to support informed decisions
about aircraft deployment of this technology. To predict aerosol size
distributions we apply microphysical parameterizations of nucleation,
condensation and coagulation to simulate an aerosol plume generated via
injection of calcite powder or sulphate into a stratospheric wake with
velocity and turbulence simulated by a three‐dimensional (3D) fluid dynamic
calculation. We apply the model to predict the aerosol distribution that
would be generated by a propeller wake in the Stratospheric Controlled
Perturbation Experiment (SCoPEx). We find that injecting 0.1 g s‐1 calcite
aerosol produces a nearly monodisperse plume and that at the same injection
rate, condensable sulphate aerosol forms particles with average radii of
0.1 µm at 3 km downstream. We test the sensitivity of plume aerosol
composition, size, and optical depth to the mass injection rate and
injection location. Aerosol size distribution depends more strongly on
injection rate than injection configuration. Comparing plume properties
with specifications of a typical photometer, we find that plumes could be
detected optically as the payload flies under the plume. These findings
test the relevance of in situ sampling of aerosol properties by the SCoPEx
outdoor experiment to enable quantitative tests of microphysics in a
stratospheric plume. Our findings provide a basis for developing predictive
models of SAI using aerosols formed in stratospheric aircraft wakes

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