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of runoff
Following the principles of runoff-collecting forestry and applying the forest structure investigation results, the authors developed a formula to calculate appropriate density for forests on the basis of different diameters at breast height (DBH).
      
This technique is used to construct a model of runoff transformation for fragments of the Volga basin.
      
Methods of the use of radar information in applied hydrology (in particular, for calculation of runoff probability) are developed.
      
The anthropogenic components of runoff dynamics from drained fields are calculated.
      
However, some components of the total runoff into the Arctic Ocean feature distinct and fairly complicated disturbances in the homogeneity of runoff variations.
      
Rivers of the northwestern America and northeastern Asia featured a regular increase in the amplitude of runoff variations and their autocorrelation since the late 1960s.
      
The simulation of runoff from small catchments in the permafrost zone by the SWAP model
      
The dynamics of runoff from a watershed is considered based on the momentum balance equation.
      
Soil moisture in spring is decreased because of the reduction of infiltration and increment of runoff.
      
Between October 1998 and October 2000, due to an inadequate supply of runoff and sediment, about 1.4×108m3 of sediments was eroded and transported offshore.
      
Long-term ensemble forecast of snowmelt runoff with the help of the physics-based models of runoff generation
      
Applicability of the physically based models of runoff generation has been shown for the long-term ensemble forecasts of snowmelt runoff volumes and peak discharges.
      
A physical picture of runoff and disintegration in the edge wake has been obtained for subsonic, near-sonic, and supersonic wet-steam flows.
      
The experiment reuslts on detention of precipitation, permeability of stand soil water holding capacity, formation and regulation of runoff are discussed in the this paper.
      
(3) It is proved that the interflow and groundwater runoff are the major forms of runoff occured in larch forest land.
      
Review of runoff forestry in Shanxi Province and sustainable development tactics of forestry
      
The development of runoff forestry in Shanxi Province was summarized and the sustainable development tactics was put forward.
      
pseudoacacia stand and its clearcut area in the western Liaoning Province (18°50'-122°25' E, 40°24'-42°34' N) for measuring the characteristics of runoff and sediment as well as soil moisture dynamics.
      
Contractive analysis of the two land types showed that there existed a significant difference in volumes of runoff and sediment between the sites ofR.
      
Hydrograph of surface runoff of typical rainfall showed that the peak value of runoff inR.
      
 

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