
Ganga's summer flow sustained by groundwater, not glacial melt: IIT Roorkee study
The study established the negligible role of glacier melt in maintaining the Ganga's summer flow, quantifying that beyond the Himalayan foothills, glacier-fed input is virtually absent and does not influence the summer discharge up to Patna. After Patna, tributaries such as the Ghaghara and Gandak become the dominant contributors, the study noted.
The findings were published in Hydrological Processes, a peer-reviewed American journal.
The study monitored river flow and its controlling factors such as evaporation loss, groundwater interaction, and the role of aquifer water levels in sustaining river flow. It employed isotope ratio (composition) techniques using a cavity ring-down spectrometer. Six laboratories, including one from Taiwan, assisted with various measurements required for the research.
Moreover, researchers found that in the upstream region of around 160 km, no significant change in isotopic composition was observed, indicating minimal evaporation due to the fast flow of water along a relatively steep gradient.
The negligible fluctuation in isotope values indicates limited interaction with groundwater, contrary to earlier satellite-based studies that warned of severe groundwater depletion across North India.
"In-situ groundwater level data show that the water table in the middle plain region of the Ganga has not changed significantly in recent decades to affect the summer base flow of the river. Our analysis shows that the Ganga is not drying because groundwater is depleting, but due to over-extraction, excessive diversion, and neglect of tributaries. Groundwater is still the hidden lifeline of the Ganga," said Professor Abhayanand Singh Maurya, lead author from the institute's Earth Sciences department.

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