Sentence examples for ratio of stream from inspiring English sources

Rho coefficient is defined as ratio of stream length ratio and bifurcation ratio (Horton 1945).

However, the ratio of stream to parent-node variance emerges as a better predictor of variance reduction for individual streams, particularly in complex network structures.

Arctic watersheds (Mackenzie and Yukon Rivers) had a relatively elevated ratio of stream load to atmospheric deposition (0.27 and 0.74), possibly because of melting glaciers or permafrost releasing previously stored Hg to the streams.

The stream NO3− concentration was significantly correlated with the upland (grassland and cropland) proportion of the catchment's area, and the ratio of stream NO3− concentration to this proportion tended to be lower in low-elevation areas, indicating higher NO3− denitrification.

In quasi LP model continuous variables are regrouped into (a) normal variables such as concentration, temperature and flow rate (b) variables which make the equations nonlinear such as conversion in each reactor, split ratio of streams, recycles and exit temperatures from coolers or heaters.

In the non-Arctic regions, watersheds with natural vegetation tended to have low ratios of stream load to Hg deposition (< 0.1), whereas urbanized areas had higher ratios (0.34 1.0) because of impervious surfaces.

Mean stream length is the ratio of total stream length of particular order to the total number of same ordered stream and is denoted by (L_{{{bar{text{u}}}}}) (Fig. 3).

The signal-to-noise-interference ratio (SINR) of stream i of receiver k is calculated as begin{array}rcl@ text{SINR}_{ki} = frac{left(mathbf{d}_{k}^{i}right)^{H}mathbf{H}_{kk}mathbf{t}_{k}^{i}left(mathbf{t}_{k}^{i}right)^{H}mathbf{H}_{kk}^{H}mathbf{d}_{k}^{i}}{left(mathbf{d}_{k}^{i}right)^{H}mathbf{B}_{ki}mathbf{d}_{k}^{i}} forall k = 1,ldots,K, ::: forall i = 1,ldots,q_{k} end{array} (4).

A method of pressure tube (Pitot's tube) was proposed Shulyupin et al. (2012) as an alternative to the orifice, in which steam flow rate is determined by down-stream dynamic pressure and phase composition is determined by ratio of down-stream and up-stream dynamic pressures.

Lastly, the summer stream/air temperature ratio of a stream may be useful in assessing existing or expected stream temperature conditions at a site in relation to these factors or in identifying unique environmental conditions or potential restoration needs at a site.

The flow rate is the ratio of average stream cross section area and average time taken to fill the container.