   The balance between the water inputs and the water    outputs   Equation:     P= Q + E + S   Where:      P= precipit...
 used to help manage water supply and predict where there may be water shortages. also used in:   irrigation,   runoff...
   illustrated using a water balance graph   plots levels of precipitation and evapotranspiration   often on a monthly ...
1. Soil moisture surplus:    soil moisture is full for plant use    and run off into streams                              ...
   Annual precipitation always exceeds evapotranspiration Precipitation (Input) exceeds evt loss (output) = positive wat...
Rainfall – discharge relationship with drainage basins   lesson 4
Rainfall – discharge relationship with drainage basins   lesson 4
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Rainfall – discharge relationship with drainage basins lesson 4

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Rainfall – discharge relationship with drainage basins lesson 4

  1. 1.  The balance between the water inputs and the water outputs Equation: P= Q + E + S Where: P= precipitation Q= total streamflow (runoff) E= Evapotranspiration S= Storage (in soil & bedrock)
  2. 2.  used to help manage water supply and predict where there may be water shortages. also used in:  irrigation,  runoff assessment  flood control and  pollution control.
  3. 3.  illustrated using a water balance graph plots levels of precipitation and evapotranspiration often on a monthly scale. The graph helps to highlight river-basin management challenges, which include:  Periods when there is likely to be water deficiency or drought  Periods when flooding is most likely to occur  The best time for irrigation  Long-term changes in the storage capacity of the drainage basin  The need for a water transfer system
  4. 4. 1. Soil moisture surplus: soil moisture is full for plant use and run off into streams 2 32 Soil moisture use: plants must rely on stored 4 water which gradually used up 1 53. Soil moisture deficiency: plants must have adaptation for long periods or land must be irrigated4. Soil moisture recharge: the soil water stored start to be recharged5. Field capacity: the soil water stores are now full
  5. 5.  Annual precipitation always exceeds evapotranspiration Precipitation (Input) exceeds evt loss (output) = positive water balance soil moisture surplus However, 1974 &1975 as well as 1995 & 1996 – long dry summer  Evapotranspiration exceeds precipitation  temporary negative water balance During winter, ppt > evt = soil moisture surplus   considerable river run off & rise in river levels In summer, evt > ppt (plants & humans utilise the water from the soil storage  depletion and fall in river levels By Autumn, ppt> evt = first water surplus is to recharge the until the soil reach field capacity

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