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water budgets
show the annual balance between inputs and outputs and their impact on water availability
influenced by climate type
uses of water budgets
at both national and regional scale:
provide useful indication of the amount of water available for human use
at a local scale:
provide info about available soil water
aspects of water budgets
soil moisture deficit
soil moisture recharge
soil moisture surplus
soil moisture utilisation
soil moisture deficit
the degree to which soil moisture falls below field capacity
in temperate areas this is high in summer due to low levels of precipitation and high levels of evapotranspiration
soil moisture recharge
occurs when precipitation exceeds potential evapotranspiration
there is some refilling of water in dried-up pores of the soil
happens in autumn in temperate regions
soil moisture surplus
the period when soil is saturated and water cannot enter
so it flows over the surface
precipitation exceeds evaporation
soil moisture utilisation
process by which water us drawn to the surface through capillary action
this will occur when evaporation exceeds precipitation
so water gets used up