The water level at Trestno reached 724 cm , causing widespread devastation.

A occurs when heavy or prolonged rainfall (often combined with snowmelt) in the upper reaches of the Odra and its tributaries (such as the Nysa Kłodzka) causes water levels to rise rapidly. As this volume of water moves downstream, it forms a "wave" that eventually reaches Wrocław. The Wrocław Water Node (WWN)

To protect the city, Wrocław utilizes a complex hydraulic system called the (Wrocławski Węzeł Wodny). This system was significantly modernized following the 1997 floods and includes:

The city issues "warning levels" followed by "alarm levels" as water heights cross specific thresholds.

When a flood wave is imminent, the and city officials activate several protocols:

A massive dry polder upstream designed to "shave" the peak of the flood wave before it reaches the city.

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The water level at Trestno reached 724 cm , causing widespread devastation.

A occurs when heavy or prolonged rainfall (often combined with snowmelt) in the upper reaches of the Odra and its tributaries (such as the Nysa Kłodzka) causes water levels to rise rapidly. As this volume of water moves downstream, it forms a "wave" that eventually reaches Wrocław. The Wrocław Water Node (WWN) The water level at Trestno reached 724 cm

To protect the city, Wrocław utilizes a complex hydraulic system called the (Wrocławski Węzeł Wodny). This system was significantly modernized following the 1997 floods and includes: The Wrocław Water Node (WWN) To protect the

The city issues "warning levels" followed by "alarm levels" as water heights cross specific thresholds. The water level at Trestno reached 724 cm

When a flood wave is imminent, the and city officials activate several protocols:

A massive dry polder upstream designed to "shave" the peak of the flood wave before it reaches the city.

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