4.7 Article

Uncertainty in Future Projections of Precipitation Decline over Mesopotamia

Journal

JOURNAL OF CLIMATE
Volume 36, Issue 4, Pages 1213-1228

Publisher

AMER METEOROLOGICAL SOC
DOI: 10.1175/JCLI-D-22-0268.1

Keywords

Precipitation; Storm tracks; Climate change; Climate models

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Centuries of sufficient water supply in Mesopotamia from the Tigris and Euphrates Rivers are now threatened by diminishing freshwater resources. Climate change and population growth could worsen the water deficit in the coming decades, while near-term projections for changes in precipitation remain uncertain. However, in the later decades of this century, a decrease in wet-season precipitation over the river basins is projected with more confidence, implying a long-term drying trend over Mesopotamia. Adapting to this uncertain future and implementing global net-zero carbon emissions could help mitigate the severity of projected droughts in the region.
For millennia, Mesopotamia was blessed by enough water supplied by the Tigris and Euphrates Rivers. However, the dwindling freshwater resource is no longer enough. In the future, climate change coupled with a growing population could considerably exacerbate the current water deficit. Based on simulations by carefully selected global and regional climate models, we conclude that these river basins may possibly face further water shortages (mainly due to a reduction in spring-season precipitation) in the next few decades (2021-50) under a scenario of high emissions of greenhouse gases. However, there is no consensus among models regarding these near-term (2021-50) projections of change in precipitation, and society is likely to face the challenge of how to prepare for this uncertain future. The story is different for the late decades of this century: we project, with significantly more confidence, a robust decrease in wet-season (winter to spring) precipitation over the headwaters of these river basins, worsening future water deficits and implying a century-long drying trend over Mesopotamia. Possible physical mechanisms are proposed and discussed. As global warming progresses, higher sea level pressure, centered on the Mediterranean Sea, will likely make upstream storms less frequent and weaker, leading to drying over Mesopotamia. Further, projections show a poleward migration of the fewer Mediterranean storm tracks, decreasing the frequency of storms that penetrate into Mesopotamia. Implementing a global net-zero carbon emissions policy by midcentury could mitigate the severity of the projected droughts in this region.

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