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A tributary to East Fork of White River in Columbus, IN, is pumped dry by doubling pumping rates of nearby public water supply wells. The dry stream sections are colored gray. Under current pumping rates the tributary is flowing everywhere.
The conjunctive groundwater-surface water solution option in GFLOW is an ideal analysis tool for impacts of public or industrial pumping as well as for climate change scenarios.
Note: The wells with increased pumping rates are the pink square markers to the north-west of the tributary which runs through the town of Columbus.