Sentence examples for mean stream depth from inspiring English sources

This approach converts Sw to an uptake velocity (vi mm s−1) where vwat is mean water velocity (m s−1) and z equals mean stream depth (m).

Average flow condition theory expressed as "At-A-Station" hydraulic geometry (AHG) relations are site-specific power-functions, relating the mean stream channel forms (i.e. water depth, top-width, flow velocity, and flow area) to discharge, have been studied since 50s.

Linear aspects include stream number, stream order, stream length, mean stream length, stream length ratio and bifurcation ratio.

This critical stream depth increases with streambed thickness and decreases with stream width.

Open image in new window Fig. 5 Relation between stream order and mean stream length.

In general, it is observed that the mean stream length increases with the stream order.

According to Strahler (1964), mean stream length describes the characteristic size of components of stream network.

The mean stream N2O emissions were 0.190 mg N m−2 h−1.

The mean stream length is directly related to mean annual runoff; therefore, the highest mean stream length has relatively high mean annual rainfall runoff and relatively low mean annual rainfall runoff in less mean stream length.

The linear aspects parameters were considered about stream order (U), stream numbers (N u ), stream length (L u ), mean stream length (L sm), stream length ratio (R l), and bifurcation ratio (R b).

In the present study, mean stream length is indicating the high mean annual rainfall runoff.