Persistent monsoon rainfall across Indian-occupied Kashmir and Punjab regions is triggering a significant rise in water levels throughout the Chenab river system. Current hydrological data reveals substantial inflow imbalances, particularly in the Jhelum tributary where inflows reach 57,400 cusecs compared to controlled outflows of 10,000 cusecs. This disparity indicates accumulating water volumes that could lead to elevated river conditions and potential flood risks in downstream areas, affecting water management infrastructure and communities dependent on river systems.

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