Strategies against flood losses

The influences of mankind — in the form of impervious surfaces, river training works, and anthropogenic climate change — can trigger and exacerbate floods. Not every case of flood necessarily leads to flooding, however.

And even if flooding does occur, the losses can still be kept within reasonable bounds and do not always have to be major losses. This presupposes a suitable prevention strategy which embraces all aspects of floods, from their origins to the avoidance of loss potentials.

Little effect will be gained from concentrating on specific aspects like ecological and technical measures (e.g. river restoration and dykes) or organisational and financial mechanisms (e.g. alarm plans and insurance).

Monocausal explanations of the increase in flood catastrophes are repeatedly put forward, citing as the sole trigger impervious surfaces, for example, or river regulation, or the disappearance of natural flood retention areas, or climate change.

Such one-sided allegations do not bear critical examination, however. A much more differentiated view of the causes is required.

Prevention of floods

A flood occurs when there is significantly more water in a river, in a lake, on the ground, or below the surface than normal. Floods are a part of the natural water cycle; but mankind has ways of intervening in this cycle.

The interventions include influencing the climate (resulting in more frequent and more intense precipitation), changing the infiltration capacity of the soil (impervious surfaces, soil compacted by agriculture), discharging water into rivers and lakes (drainage ditches, sewers), and directing it towards the sea (e.g. river regulation, removal of flood retention areas).

Retaining more water must have top priority whenever possible. One thing must be noted, however: extreme floods in large catchments are not attributable to surfaces which have been made impervious by human activity; this has a relatively minor impact.

Likewise, local flood detention, river restoration, and dyke relocations can only reduce extreme flood peaks to a limited degree. We must consider the huge masses of water involved in extreme events on large rivers.

For example, the destructive section of the Mosel flood wave in the 1993 Christmas floods had a flow rate of over 2,000 m³/s and a volume of 840 million m³; a basin the size of Lake Constance with a water depth of 1.56 m would have been required to retain it. Nevertheless, even if some measures have only a limited effect, they must be encouraged and implemented.

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