For any country and climate, precision in these long-term water studies is important because an over or underestimation of future water supplies can have detrimental effects, said Dessie Nedaw Habtemariam, Associate Professor at Addis Ababa University in Ethiopia.
“If we misestimate how fast water is replenished, for example, and our estimate is too high, and then communicate these results to the decision makers, they could implement policies that result in groundwater being extracted faster than it can be recharged,” Habtemariam said. Groundwater — water in the layer of permeable rock under the earth’s surface — is a primary source of fresh water for the majority of Ethiopia’s population. “This would lead to a sharp decline in available groundwater supplies, which could mean an abandonment of boreholes and may even lead to drinking water shortages.”
Underestimation, on the other hand, could lead to unnecessarily stringent water policies or influence development decisions, such as hampering urban expansion due to a lack of water resources.
For these long-term studies of over 100 years or more, getting accurate results using other water balance models has been a major challenge, said Tricia Stadnyk, Associate Professor of water resources engineering at the University of Manitoba in Canada. “Many water balance models do a very good job at simulating the flow of water in streams, rivers and other water bodies, but are very bad at getting the amount of evapotranspiration right,” she said, referring to the process of evaporation of water from land and the movement of water from plants to the atmosphere. “For climate change predictions, this is a huge problem because one of the big things we look at is evapotranspiration.”
As temperatures become more extreme due to climate change, the rate of evapotranspiration does too. The more evapotranspiration, the less water on the earth’s surface, and vice versa. This, in turn, influences the entire annual water cycle and can lead to unpredictable extremes that swing from too little water, causing drought, to too much water, causing floods.
No climate is immune to these changes. They can affect a climate like Canada’s, where more than 60% of the land mass is some form of permafrost — frozen ground — and there are four distinct seasons, or one like Ethiopia’s, where much of the country is tropical and the temperature remains more or less constant throughout the year.
These diverse conditions can be captured by adjusting the model, which makes it globally applicable. Scientists from several countries are working with the IAEA to receive training and support in using the IAEA’s isotope-enabled water balance model and other models for improving water resource management. In Ethiopia, for example, a three-year technical cooperation project is being launched to study the upper Awash Basin — a large groundwater reservoir supplying fresh water to more than
2.6 million people. Other countries, like Canada, are setting up or have set up isotope sampling networks to improve accuracy when using models such as the IAEA’s.