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Global Water Bankruptcy Report

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Source: Down To Earth (DTE)

What is the news?

The UNU-INWEH has released a flagship report titled “Global Water Bankruptcy: Living Beyond Our Hydrological Means in the Post-Crisis Era”, warning that large parts of the world have entered a permanent state of water insolvency, where water use exceeds renewable and safe limits.

What is “Water Bankruptcy”?

  • A persistent failure state where:
    • Long-term water withdrawals exceed renewable inflows and safe depletion thresholds.
    • Results in irreversible damage to natural water capital (aquifers, rivers, wetlands).
  • The report argues that terms like “water stress” or “water crisis” are inadequate, as the earlier “normal” hydrological baseline has already collapsed in many regions.
Key Data & Findings
  • Global scale:
    • ~75% of world population lives in water-insecure or critically water-insecure countries (2026).
  • Agriculture:
    • ~70% of global freshwater used for agriculture.
    • 170+ million hectares of irrigated cropland under high or very high water stress.
  • Groundwater:
    • ~70% of major global aquifers show long-term decline.
    • Land subsidence of up to 25 cm/year in some regions.
  • Wetlands:
    • Loss of ~410 million hectares in 50 years (≈ size of the EU).
  • Economic cost:
    • Anthropogenic droughts cost $307 billion annually, more than the GDP of ~75% of UN member states.
Major Causes Identified
  • Slow-onset depletion: Chronic over-allocation and over-pumping.
    Example: Severe groundwater depletion in the Indo-Gangetic Plain.
  • Infrastructure-driven overshoot: Dams and diversions enabling unsustainable urban growth.
    Example: Inter-basin transfers supplying Chennai failing during monsoon shocks.
  • Ecological liquidation: Loss of wetlands and forests reduces recharge and flood buffering.
    Example: Bengaluru wetland degradation.
  • Climate-amplified overshoot: Climate change accelerates glacier melt and rainfall variability.
    Example: Himalayan glacier retreat threatening Indus–Ganga flows.
  • Institutional inertia: Policies assume return of old hydrological normal.
    Example: Resistance to crop diversification in water-scarce regions.

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