Heavy precipitation and snowmelt, as well as an increase in the temperature background can lead to active snowmelt and the formation of melt runoff, weakening of ice phenomena and rising water levels in rivers. These are possible floods and associated negative consequences in the form of flooding and flooding.
Flood is one of the types of floods. The reasons are: a sharp increase in the temperature background, intense melting of snow and intense rains. At the same time, in mountainous and foothill areas, the formation of slope drains is possible.
All foothill settlements are exposed to such danger, floods are formed in low places, there is an accumulation of meltwater, the groundwater level rises. First of all, those residential areas are flooded where there is no drainage and irrigation network or it is in an unsatisfactory condition.
At the same time, when heavy snowmelt occurs with a sharp increase in the temperature background, the formation of slope runoff occurs in the foothills and in low-lying places on the plain.
In conditions of frozen soil, this can lead to flooding of residential buildings and outbuildings in populated areas.
OCHS of the city of Tekeli