In summer, water flow often reduces to a trickle in many parts of India due to increased evaporation rates and high temperatures, leading to diminished water levels in rivers and lakes. Additionally, the prolonged dry season before the monsoon causes lower groundwater recharge, further depleting surface water sources. Agricultural demand for irrigation during this period also exacerbates the situation, straining available water resources. As a result, many rivers and streams experience significantly reduced flow.
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