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Water Insecurity

Water insecurity is a critical global risk intensified by climate change, threatening billions through droughts, floods, and disrupted water cycles.

Water in Crisis: Quick Facts (2026)

  • ~50% of large lakes worldwide have lost water since the early 1990s, affecting about 25% of the global population dependent on them. 
  • Around 70% of major aquifers are in long-term decline, indicating widespread groundwater depletion. 
  • About 410 million hectares of wetlands (nearly the size of the EU) have been lost over the past 50 years, with an estimated US$5.1 trillion annual loss in ecosystem services. 
  • Roughly 75% of humanity lives in water-insecure or critically water-insecure countries.  
  • About 4 billion people face severe water scarcity for at least one month per year, and 2.2 billion lack safely managed drinking water.  
  • Around 3.5 billion people lack safely managed sanitation services globally.  
  • Approximately 170 million hectares of irrigated cropland are under high or very high water stress, threatening global food systems.  
  • Around 3 billion people live in areas where total water storage is declining or unstable, regions that also produce more than half of global food.  
  • The global economic burden of drought is estimated at ~US$307 billion per year.  
  • About 1.8 billion people experienced drought conditions (2022–2023) linked to both climate and human water overuse. 
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Annual Precipitation Loss

Water Insecurity

The map above shows areas with annual precipitation loss under the 1° C above the 1850‐1900 average scenario, which we already passed in 2017. Explore more about the changes in global precipitation distribution under other scenarios presented in Probable Futures’ predictions.

According to the latest Met Office outlook, global temperatures are projected to stay above 1.4°C relative to pre-industrial levels in 2026, continuing a recent run of exceptionally warm years influenced by both long-term human-driven warming and natural variability. This means the scenario shown on the map is already broadly representative of present-day climate conditions rather than a future projection. 

Explore more about the changes in global precipitation distribution under other scenarios presented in Probable Futures’ predictions. 

Climate Change Intensifies Water Cycle Disruption

Climate change is having a significant impact on water availability by changing hydrological and meteorological conditions – changes in the water cycle, melting glaciers and ice, unpredictable precipitation, increasing evapotranspiration (the sum of evaporation from the land surface plus transpiration from plants), and drying water bodies. The poles feed into the global climate system through the albedo effect (the ability of Earth’s surfaces to reflect the sun’s rays back to the atmosphere), a warmer Arctic and Antarctic with less ice and snow will darken the Earth, causing more of the sun’s heat to be absorbed. This, in turn, will fuel extreme weather events such as heatwaves, flooding and drought – all of which disrupt the water cycle and exacerbate water insecurity.

Water Shortages

Sea level rise from melting glaciers in Greenland increases the risk of saltwater intrusion into freshwater supplies. This in turn threatens both food and water security, as highlighted in our Pacific region stories. Extreme drought, such as that experienced in Europe in summer 2022, also has a huge impact on water availability. Other regions at high risk of drought include large parts of Africa, Southeast Asia, and the west coast of the USA.

In East Africa (Feb 2026), drought conditions affected around 4.6 million people and displaced over 135,000 in Somalia alone, with widespread crop and livestock losses linked to persistent soil moisture deficits. 

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Group of children gathering water from a well in Kitgum, Uganda. Credit: illustrate Digital Ug, Pexels.
In Cyprus (Feb 2026), reservoir levels fell to just 13.7% of total capacity, the lowest recorded since hydrological monitoring began in 1901, signaling extreme long-term water stress in the Eastern Mediterranean.

Melting snow and glaciers in the Himalayas have also resulted in changes in the seasonality of the hydrological cycle. These cause significant problems for agriculture, hydroelectric power distribution, and drinking water supplies in urban and rural centres that rely on meltwater.

The ICIMOD HKH Snow Update 2026 reports a strong and sustained decline in seasonal snow across the Hindu Kush Himalaya. Snow persistence is 27.8 percent below the long-term average, which is the lowest level in over two decades and the fourth consecutive year of below-normal conditions. This decline is widespread across major river basins and reduces natural water storage in the region’s mountain “water towers” that support nearly two billion people downstream. Reduced snowpack is expected to lower spring and early summer river flows, increasing pressure on water availability for agriculture, hydropower, and household use. The report warns that these changes are already intensifying drought stress and increasing water insecurity across the region.  

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Hindu Kush Himalayas. Credit: Mysara Hassan, Pexels.

Tehran faced an acute water crisis in late 2025, when an Iranian water official reported that storage across the city’s five main dams had fallen to about 170 million cubic meters, roughly half the level recorded at the same time the previous year. Authorities also noted that Iran was experiencing its most prolonged drought in six decades, with rainfall down by around 96 percent compared with the same period the year before. This sharp decline in precipitation and multi-year drought conditions has continued to drive historically low reservoir levels and sustained pressure on urban water supply systems into 2026. 

In the Caribbean (June 2026), St Lucia is facing a worsening water crisis, with water authorities reporting that water production in several supply systems has fallen by up to 60% and source capacity is below 50% in some areas, despite the onset of the rainy season. Low inflows, aging infrastructure, and climate variability are limiting recovery even during expected wet periods, forcing reliance on water storage tanks and managed supply restrictions. 

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