A winterbourne is a stream that occurs in the upper reaches of a river fed by a chalk aquifer. The winterbourne flows in the winter typically from December until approximately April before declining until the following winter. When it rains, the porous chalk holds water in its aquifer and releases the water at a steady rate. During the dry season, the water table can fall below the level of the stream bed, causing it to dry up. The length of the dry phase depends on the longitudinal position of the stream.