Sentence examples for stream basin area from inspiring English sources

The basic parameters like length of individual stream, basin area, and perimeter of the basin were extracted from the Arc GIS-10 geodatabase and further used for calculating morphometric parameter such as linear, areal, relief, and tectonic aspects by means of various equations (Table 1).

Evaluation of morphometric parameters could be calculated from the analysis of various drainage parameters such as ordering of the various streams and basin area, perimeter and length of drainage channels, drainage density, stream frequency, bifurcation ratio, texture ratio, basin relief, ruggedness number, and time of concentration (Kumar et al. 2000; Nag and Chakraborthy 2003).

Information on number of different orders of streams, stream length and corresponding basin area etc. were extracted from the vectorized maps.

Hack (1957) identified that for a large number of basins, the stream length and basin area is associated by a simple power function as follows: Lar = 1.4* × A0.6.

To evaluate the drainage basin morphometry, various parameters like stream number, stream order, stream length, stream length ratio, bifurcation ratio, basin length, basin area, relief ratio, elongation ratio, drainage density, stream frequency, form factor and circulatory ratio, etc., have been analysed using the standard mathematical formulae given in Table 1.

Evaluation of morphometric parameters requires the analysis of various drainage parameters such as ordering of the various streams, measurement of basin area and perimeter, length of drainage channels, drainage density (Dd), bifurcation ratio (Rb), stream length ratio (RL), and relief ratio (Rh).

To evaluate the basin morphometry, various parameters like stream number, stream order, stream length, stream length ratio, bifurcation ratio, basin length, basin area, relief ratio, elongation ratio, length of overland flow, drainage density, stream frequency, drainage texture, form factor and circulatory ratio have been analysed using the standard mathematical formulae given in Table 1.

The first order streams account for 61.33% of the total stream numbers in the basin area.

Also, basin area, stream network, and precipitation seasonality are found to be the most effective explanatory variables in prediction modeling by the QRT and PRT.

The development of stream segments in the basin area is more or less effected by rainfall.

The development of stream segments in the basin area is more or less affected by rain fall.