Sentence examples for depth of precipitation from inspiring English sources

As it is shown in Fig. 16, if production rate is increased, the depth of precipitation process will be reduced.

The natural resource conservation service curve number approach was used to estimate the initial abstraction of precipitation, infiltration, runoff, and estimate the threshold depth of precipitation.

As shown in Fig. 19, as the tubing diameter increases from 3 to 7 inches, the precipitation interval reduces about 2500 ft. In addition, a greater increase in the tubing size results in more depth of precipitation initialization.

The choke size results in the same effect on the depth of precipitation initiation as the production rate does because generally, an increase in choke size is directly proportional to the production rate.

As a matter of fact, in this case, as the tubing diameter increases from 3 to 7 inches, the precipitation interval reduces about 2500 ft. In addition, a greater increase in the tubing size results in more depth of precipitation initiation.

To calculate mean monthly rainfall of the study area, data from the metrological station were used using the arithmetic mean which is given below: frac{{p = p_{1} + p_{2} + p_{3} ldots p_{n} }}{N} (1 where P is the average depth of precipitation of the area, P 1, P 2, P 3 and P n are the rain fall records at stations 1, 2, 3, and N is the number of metrological stations.

Graphical outputs include time series plots of precipitation depth, partitioned run-off volumes, watertable depth (average or TI/STI based), and map graphics of TI, STI, and depth to watertable.

The contribution of precipitation depth change has little correlation with the aridity index, while positively correlates to the significance of trend in precipitation depth.

The δ13C and δ18O compositions of sand calcites are a function of precipitation depth in relation with the warming of surface water during infiltration.

In this paper, annual maxima series of precipitation depths obtained from daily rainfall data measured at three selected stations in southeast UK are analysed using a range of probability distributions.

Nitrogen depth profiles calculated on the basis of precipitation agree reasonably well with experimentally observed depth profiles, except for the occurrence of a tail advancing the main nitriding front, which is obtained in the calculations, but is not observed in the experiment.