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The Thornthwaite equation (water balance) is a simple, yet useful index, for one can calculate amounts of surplus (runoff) and deficit (not enough soil moisture)
The Thornthwaite equation (water balance) is a simple, yet useful index, for one can calculate amounts of surplus (runoff) and deficit (not enough soil moisture) in surface water (i.e. changes in storage, streamflow), simply by comparing ________ with _____________
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