Research reveals over half of the world’s groundwater flows could take over 100 years to respond fully to climate change Future generations could be faced with an environmental ‘time bomb’ if climate change is to have a significant effect on the world’s essential groundwater reserves.
In a new paper published in the journal Nature Climate Change, the research team have shown that in more than half of the world’s groundwater systems, it could take over 100 years for groundwater systems to completely respond to current environmental change.
Groundwater found underground in the cracks and pore spaces in soil, sand and rock, is the largest source of usable freshwater in the world and is relied on by more than two billion people as a source of drinking and irrigation water.
Groundwater resources are replenished predominantly through rainfall in a process known as recharge.
If there is a change in recharge, for example, due to a reduction in rainfall as a result of climate change, the levels of water in the ground will begin to change until a new balance is achieved.
Lead author of the research, Dr Mark Cuthbert, from Cardiff University’s School of Earth and Ocean Sciences and Water Research Institute, said: “Our research shows that groundwater systems take a lot longer to respond to climate change than surface water, with only half of the world’s groundwater flows responding fully within ‘human’ timescales of 100 years.
“This means that in many parts of the world, changes in groundwater flows due to climate change could have a very long legacy.
This could be described as an environmental time bomb because any climate change impacts on recharge occurring now, will only fully impact the baseflow to rivers and wetlands a long time later.
They discovered that, in general, groundwater in wetter, more humid locations may respond to climate change on much shorter timescales, whereas more arid locations where water is more scarce naturally have much longer groundwater response times.
The pinpointing of locations is significant as for many parts of the world, especially where surface water supplies are less available, the domestic, agricultural, and industrial water needs can only be met by using the water beneath the ground.