India opens Salal Dam gates as heavy rains raise Chenab flood fears

Heavy monsoon rains in Indian-administered Kashmir have caused a sharp rise in the water level of the

Heavy monsoon rains in Indian-administered Kashmir have caused a sharp rise in the water level of the Chenab River, prompting India to open all seven gates of the Salal Dam.

According to reports, the dam gates were opened without prior notification to Pakistan. The sudden release of water has increased the flow in the Chenab River, with the surge now moving downstream toward Head Marala in Pakistan. The distance between the Salal Dam and Head Marala is approximately 72 kilometers.

The rapid increase in river flow has raised concerns among Pakistani authorities, who are closely monitoring the situation. Officials fear that if water levels continue to rise, downstream areas could face flooding.

The Indian Meteorological Department has forecast more rainfall in several parts of Indian-administered Kashmir during the next few hours. The weather system is expected to keep water inflows into rivers and reservoirs at a high level.

Experts warn that continued rainfall may significantly increase the volume of water in the Chenab River. If the rain persists, flood conditions could worsen over the next 24 to 36 hours.

The possibility of a serious flood situation has prompted authorities to remain on alert. Relevant departments are monitoring river levels and assessing the potential impact on vulnerable areas along the Chenab.

The developing weather conditions have also increased concerns for communities living near the river, particularly in low-lying areas that are more vulnerable to rising water levels. Officials are expected to continue monitoring the situation and take precautionary measures if river flows increase further.

The flood risk will largely depend on the intensity of rainfall in the upper catchment areas over the coming hours. Any additional heavy downpours could further increase pressure on the river system and raise the likelihood of flooding in downstream regions