https://esd.copernicus.org/preprints/esd-2023-6/

*Authors*
Chencheng Shen, John C. Moore <[email protected]>, Heri Kuswanto,
and Liyun Zhao

*Received: 02 Mar 2023 *

*Discussion started: 07 Mar 2023*

Abstract

The Indonesia Throughflow (ITF) is the only low-latitude channel between
the Pacific and Indian oceans, and its variability has important effects on
global climate and biogeochemical cycles. Climate models consistently
predict a decline in ITF transport under global warming, but it has not yet
been examined under solar geoengineering scenarios. We use standard
parameterized methods for estimating ITF: the Amended Island Rule and
Buoyancy Forcing, to investigate ITF under the SSP2-4.5 and SSP5-8.5
greenhouse gas scenarios, and the geoengineering experiments G6solar and
G6sulfur that reduce net global mean radiative forcing from SSP5-8.5 levels
to SSP2-4.5 levels using solar diming and sulfate aerosol injection
strategies. Six model ensemble mean projections for 2080–2100 relative to
historical ITF are reductions of 19 % under the G6solar scenario and 28 %
under the G6sulfur scenario which compare with reductions of 23 % and 27 %
under SSP2-4.5 and SSP5-8.5. Thus, significant weakening of the ITF occurs
under all scenarios, but G6solar closer approximates SSP2-4.5 than does
G6sulfur. In contrast with the other three scenarios which show only
reductions in forcing due to ocean upwelling, the G6sulfur experiment shows
a large reduction in ocean surface wind stress forcing accounting for 47 %
(38 %~65 % across model range) of the decline of total ITF transport. There
are also reductions in deep-sea upwelling in extratropical western boundary
currents.
How to cite. Shen, C., Moore, J. C., Kuswanto, H., and Zhao, L.: The
Indonesian Throughflow Circulation Under Solar Geoengineering, Earth Syst.
Dynam. Discuss. [preprint], https://doi.org/10.5194/esd-2023-6, in review,
2023.

*Source: EGU GENERAL ASSEMBLY 2023*

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