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Water Balance

The water balance is the accounting exercise that quantifies all water inputs, outputs, and storage changes within a system—a river basin, a country, a company, or even an urban ecosystem—over a specified period. Just as a financial balance sheet reveals economic health, the water balance reflects the security and sustainability of the resource, identifying surpluses, deficits, and trends that guide decision-making.

Why it is crucial

  • Drought planning: a sustained deficit of > 10% for three years predicts severe restrictions, according to the Segura River Basin Authority.
  • Infrastructure sizing: hydropower plants, desalination facilities, and aquifer-recharge systems are designed based on up-to-date balances.
  • Transboundary negotiations: the 2022 Guadiana Treaty relied on joint balances to establish minimum ecological flows.

Calculation methods

  • Hydrometeorological observation: data from rain gauges, streamflow stations, and satellites (SMOS, GRACE).
  • Hydrological models (SWAT, WEAP): integrate land use and climate change.
  • Remote sensing: MODIS sensors for estimating actual evaporation.

Modern estimation methods

  • In-situ observation: rain gauges, lysimeters, and gauging stations.
  • GRACE and SMOS satellites: detect changes in groundwater and soil moisture with an error < 2 cm water equivalent.
  • Integrated hydrological models: WEAP and SWAT, calibrated with land-use data and projected climate variables.

Application example

In the Guadalquivir Basin (Spain), the 2023 water balance showed:

  • Precipitation (P): 450 mm/year
  • Evapotranspiration (E): 520 mm/year
  • Runoff (Q): 110 mm/year
  • ΔS: –40 mm/year (groundwater decline)

Result: a deficit of –220 mm/year; the Special Drought Plan was activated, reducing agricultural allocations by 25%.

Trends under climate change

Our 10-year analysis reveals that Spanish Mediterranean basins lose an average of 6 mm of P per decade and gain 8 mm of E, widening the regional hydrological deficit. These values require adjusting annual balances and basin-management plans.

Strategies to rebalance the water budget

  • Smart agriculture: soil-moisture sensors and fertigation reduce water use by 30%.
  • Urban water reuse: Valencia tripled its reclaimed water to 120 hm³ (2015–2023).
  • Renewable-powered desalination: photovoltaic-driven reverse osmosis achieves a net cost of €0.45/m³ and a carbon footprint of 0.22 kg CO₂e/m³.
  • Managed aquifer recharge: 40 km of infiltration trenches replenish 60 hm³/year.
  • Progressive pricing: tiered tariffs reduce domestic consumption by 12% in Barcelona.

Relationship with other concepts

  • Water stress: measures pressure on resources; directly derived from a negative balance.
  • Blue water scarcity: compares the blue water footprint with availability calculated in the balance.
  • AWARE: indicator that weights water consumption according to local scarcity using global hydrological-balance data.
  • Water neutrality: requires first quantifying the internal balance before offsetting.

The water balance is the cornerstone of hydrological planning. A sustained deficit of just 5% over five years triggers a chain reaction: piezometric decline, aquifer salinisation, and collapse of high-value crops. Adaptive management, investment in efficiency, and source diversification are the only pathways to restoring a region’s blue accounting.

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Related terms

Blue Water Footprint

The blue water footprint represents the volume of surface and groundwater withdrawn from rivers, lakes, reservoirs, and aquifers to produce goods and services.

Blue Water Scarcity

Blue water scarcity is an indicator that compares the consumption of surface and groundwater resources (blue water footprint) with the availability of renewable freshwater within a river basin over a specific period.

Blue carbon

Blue carbon refers to the carbon stored in coastal and marine ecosystems, such as mangroves, seagrass meadows, and salt marshes.

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