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La Plata Basin_ESA_Camilloni1

La Plata Basin Hydroclimate Response to Solar Radiation Modification with Stratospheric Aerosol Injection

Modelling
Argentina | Camilloni
Extreme weather, Hydrology

Summary

Solar radiation modification (SRM) using stratospheric aerosols could limit warming in South America’s La Plata Basin to under 1°C, compared to over 3°C under high emissions. It would reduce extreme heat and heavy rainfall, improve river flows, and ease drought risks. However, SRM also alters rainfall patterns, with some areas getting wetter, creating uncertainties. While it may lessen climate extremes, SRM is not a perfect fix and carries potential side effects.

Abstract

This study analyses the La Plata Basin (LPB) hydroclimate response to Solar Radiation Modification (SRM) with Stratospheric Aerosol Injection (SAI) in terms of changes in mean and extreme temperature, rainfall, and river flows simulations from the Geoengineering Large Ensemble (GLENS). The GLENS data used consists of three members simulations of a single model under the high anthropogenic emission scenario RCP8.5 with and without sulfur injection in the tropical stratosphere. The response of such an intervention is compared to a historical period (1980–2010) and to projections under the RCP8.5 scenario for two time slices: 2021–2050 and 2051–2080. The analysis of changes in extreme temperature and precipitation focuses on a subset of climate indices from the Expert Team of Climate Change Detection and Indices (ETCCDI). To determine the possible effects of SRM in the LPB water cycle, we use the distributed Variable Infiltration Capacity (VIC) hydrologic model in combination with daily extreme temperature and precipitation outputs from GLENS. Systematic errors in both fields were corrected by the application of a statistical bias correction method. Results show robust impacts on the water cycle of the LPB due to SRM implementation, particularly associated with increased precipitation over the northern part of the region and a general reduced warming compared to the RCP8.5 scenario. These variations would lead to regional-dependent responses in the river flows, mostly related to reductions in the severity of the extremely low flow conditions. Additionally, under the SRM scenario a reduction in extreme precipitation and a cooling effect on extreme temperatures could be expected over the LPB.

Publication data

Journal: Frontiers in Climate
Date: 26 April 2022
DOI: 10.3389/fclim.2022.763983

Authors

Inés Camilloni

University of Buenos Aires & CONICET

Natalia Montroull

University of Buenos Aires & CONICET

Carla Gulizia

University of Buenos Aires & CONICET

Ramiro Saurral

University of Buenos Aires & CONICET

The Degrees Initiative
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