Groundwater Feedbacks on Climate Change in the CNRM Global Climate Model

Groundwater and climate interact in a two-way manner. Precipitation ultimately controls groundwater recharge and, conversely, groundwater may influence climate through evapotranspiration. Yet very few global climate models or Earth system models actually simulate groundwater flows. And while the expected impacts of climate change on groundwater resources are the subject of a growing concern, global-scale groundwater-climate feedbacks have received very little attention so far. Here we show that the integration of unconfined aquifers in a global climate model can region-ally affect the climate change signal on temperatures and precipitation. We assess the impact of groundwater under preindustrial and 4xCO2 conditions (after climate stabilization). In both cases, we find that groundwater has a cooling and a wetting effect in certain regions of the world. In eastern Europe, both these impacts are stronger in the warmer climate (4xCO2 forcing) where the presence of groundwater reduces the frequency of summer heatwaves by 40%, compared to a 15% reduction in the preindustrial world. This work constitutes one of the very first global assessments of the potential feedbacks of groundwater on climate change. Our results support the idea that groundwater should be represented in global climate models and Earth system models, as it does indeed play an active role in the climate system.

Automated summary

Groundwater and climate have a two-way interaction. Global climate models rarely simulate groundwater flows, and the feedbacks between global-scale groundwater and climate have been largely ignored. This study shows that incorporating unconfined aquifers in a global climate model can regionally affect temperature and precipitation changes. Groundwater has a cooling and wetting effect in certain regions, with a stronger impact under warmer climate conditions.