Climate Change Impacts on Groundwater Systems

The hydrologic cycle is strongly controlled by climate. Therefore, changes in climate can be expected to influence water cycles and water stores globally. Our research has focused primarily on understanding the potential impacts of climate change on groundwater systems, specifically groundwater recharge, the interactions between groundwater and surface water, and the security of water.

We have conducted many modeling studies in British Columbia, including the Grand Forks aquifer, the Abbotsford-Sumas aquifer, the Okanagan Valley, and the Gulf Islands . The study areas represent a range of current hydroclimatic regimes (see map), spanning wet to semi-arid to arid, and focus on both alluvial aquifers and bedrock aquifers. The same overall methodology and computer codes were used to assess climate change impacts in each aquifer system, although over the course of these studies we refined our techniques, bringing in greater spatial resolution, a wider selection of global climate models and downscaling methods, and more rigorous modeling techniques.

map

Lower flows and extended low flow periods during the late summer and early autumn are of particular concern as they threaten not only water supplies, but also the health of wetlands and aquatic habitats. Combined with an increasing water demand due to a rapidly growing population, this is a cause of concern, particularly for the southern part of BC. With extended low flow periods, streams may be more strongly influenced by interaction with groundwater.

 

Climate Change Action Fund (CCAF) Reports:

(Allen et al., 2004) Climate Change and Groundwater: A Modelling Approach for Identifying Impacts and Resource Sustainability in the Central Interior of British Columbia (.pdf)

(Moore et al., 2007) Climate Change and Low Flows: Influences of Glaciers and Groundwater (.pdf)

 

The figure above shows a series of maps of simulated groundwater levels in the Grand Forks aquifer. The left column shows the difference in groundwater levels projected for the 2020s for different days of the year relative to current groundwater levels. The right column shows the results for the 2050s. During the spring (e.g. day 131) groundwater levels are projected to be higher on the same day of the year due to higher streamflows from earlier snowmelt. During the late summer (e.g. day 180) groundwater levels are projected to be lower. This aquifer is strongly influenced by flows in the Kettle River and the aquifer generally responds synchronously with river stage (Scibek, Allen and Whitfield, 2007: Journal of Hydrology)

Recharge to aquifers was simulated in the Abbotsford-Sumas aquifer (BC and WA) using climate data projections from four global climate models (GCMs). The figure above shows the difference in projected mean annual recharge for three future time periods based on these four GCMs. The results point to the high uncertainty in GCM projections and the need to consider a range of GCMs when making hydrologic predictions. (Allen, Cannon, Toews and Scibek, 2010: Water Resources Research).