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Data · dataset · 2026

First simulations of designing stratospheric sulfate aerosol geoengineering to meet multiple simultaneous climate objectives

Listed in National Center for Atmospheric Research

We describe the first simulations of stratospheric sulfate aerosol geoengineering using multiple injection locations to meet multiple simultaneous surface temperature objectives.

Description

Simulations were performed using CESM1(WACCM), a coupled atmosphere-ocean general circulation model with fully interactive stratospheric chemistry, dynamics (including an internally generated quasi-biennial oscillation), and a sophisticated treatment of sulfate aerosol formation, microphysical growth, and deposition.

The objectives are defined as maintaining three temperature features at their 2020 levels against a background of the RCP8.5 scenario over the period 2020-2099. These objectives are met using a feedback mechanism in which the rate of sulfur dioxide injection at each of the four locations is adjusted independently every year of simulation. Even in the presence of uncertainties, nonlinearities, and variability, the objectives are met, predominantly by SO2 injection at 30 degrees N and 30 degrees S. By the last year of simulation, the feedback algorithm calls for a total injection rate of 51Tg SO2 per year.

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The injections are not in the tropics, which results in a greater degree of linearity of the surface climate response with injection amount than has been found in many previous studies using injection at the equator. Because the objectives are defined in terms of annual mean temperature, the required geongineering results in overcooling during summer and undercooling during winter. The hydrological cycle is also suppressed as compared to the reference values corresponding to the year 2020.

The demonstration we describe in this study is an important step toward understanding what geoengineering can do and what it cannot do.

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National Center for Atmospheric Research86751e84-1426-4052-aba5-4267f05c89d710 d agoJSON v1
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