In the article the short analysis of the state of question in the area of calculations of maximal flow on territory of Mountain Crimea is presented. On the modern information a regional method is specified for the calculation of maximal runoff of rain floods.
One of basic parameters of formula of maximum intensity is considered -transformation function. The new method of determination of duration of slope influx, based on onemodal form of slope hydrograph which is approved on the rivers of left-bankness of Dnestr given about a maximal flow, is offered.
The results of a complex estimation of influence of a wood on size of the maximal runoff of floods on the rivers of Zakarpatye are resulted.
The settlement meanings of the characteristics of slope inflow are received during a spring high water on the rivers of a Podolsk height. The estimation of influence of the local factors on of slope inflow and generalization of this parameter on territory is executed.
The scientific – methodical recommendations concerning spatial generalization of the characteristics of spring flood runoff on an example of the rivers of a Podolsk height are given.
In the article the new approach to normalizing of the characteristics of the maximal runoff of flood resulting from rain for rivers of Prichernomorskaya lowland is.
In article the calculation variant of the maximal runoff formula from small river catchments is considered.
The theoretical aspects of forming of maximal flow of floods and high waters, and also possibility of construction of calculation-normative structures are expounded in the article.