https://egusphere.copernicus.org/preprints/2024/egusphere-2024-1031/

*Authors*
Philip Rasch, Haruki Hirasawa, Mingxuan Wu, Sarah Doherty, Robert Wood,
Hailong Wang, Andy Jones, James Haywood, and Hansi Singh

*How to cite*. Rasch, P., Hirasawa, H., Wu, M., Doherty, S., Wood, R.,
Wang, H., Jones, A., Haywood, J., and Singh, H.: A protocol for model
intercomparison of impacts of Marine Cloud Brightening Climate
Intervention, EGUsphere [preprint],
https://doi.org/10.5194/egusphere-2024-1031, 2024.

*Received: 05 Apr 2024 – Discussion started: 16 Apr 2024*

*Abstract*
A modeling protocol is introduced (defined by a series of model simulations
with specified model output). The protocol is designed to improve
understanding of climate impacts from Marine Cloud Brightening (MCB)
Climate Intervention. The model simulations are not intended to assess
consequences from a realistic MCB deployment intended to achieve specific
climate targets but instead to expose responses produced by MCB
interventions in 6 regions with pervasive cloud systems that are often
considered as candidate regions for such a deployment. A calibration step
involving simulations with fixed sea surface temperatures is first used to
identify a common forcing, and then coupled simulations with forcing in
individual regions and combinations of regions are used to examine climate
impacts. Synthetic estimates constructed by superposing responses from
simulations with forcing in individual regions are considered as a means to
approximate the climate impacts produced when MCB interventions are
introduced in multiple regions.

A few results comparing simulations from 3 modern climate models (CESM2,
E3SMv2, UKESM1) are used to illustrate similarities and differences between
model behavior and the utility of estimates of MCB climate responses that
have been synthesized by summing responses introduced in individual
regions. There are substantial differences in the cloud responses to
aerosol injections between models, but the models often show strong
similarities in precipitation and surface temperature response signatures
when forcing is imposed with similar amplitudes in common regions.


*Source: EGUsphere *

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