Sentence examples for streamflow exhibited from inspiring English sources

Baseflow recession rates and antecedent streamflow exhibited a negative power-law relation, with baseflow recession rates decreasing by up to two orders of magnitude as antecedent streamflow levels increased.

Three Principal Components (PCs) explained 82.4% of the variation among basin physiographic properties, and several runoff metrics (magnitude and timing of annual minimum daily runoff, mean number of days per year with 0 streamflow) exhibited significant relationships with one or more PC.

TDP streamflows exhibit significant seasonal variation with low-flow season (from November to April of the next year) accounts for only approximately 13%% of the annual total flow volume (Hsieh et al. 2014).

In contrast, over the western US, both precipitation and streamflow exhibit strong seasonality with respective monthly peaks occurring in early and late winter months.

While the distribution of mean monthly precipitation is uniform throughout the year over most of the eastern United States (except peninsular Florida), mean monthly streamflow exhibits pronounced seasonality with peak runoff occurring during the winter early springg) over the Southeast (Mid-Atlantic and Northeast) regions.

Mean rainfall and streamflow rates exhibit a pronounced inter-annual variability across the last century, though in the absence of clear sustained drifts.

Results of our analysis illustrate that information content measures of streamflow time series are much smaller than those for precipitation data, and the streamflow data also exhibit higher complexity, suggesting that the watersheds effectively act as filters of the precipitation information that leads to the observed additional complexity in streamflow measures.

The degree distribution results (Fig. 8) suggest that the annual streamflow network exhibits exponential distribution or power-law (scale-free) distribution or a combination of both, depending on the correlation threshold level considered for studying connections in the network.

Streams represented by the first annual factor occurred in southern Wisconsin and the lower peninsula of Michigan, and exhibited a linear increase in mean annual streamflow over the 33 year period caused by increased autumn and winter runoff.

Streamflow and lake level exhibit significant increasing trend for more than three-quarter of events investigated.

All drought indices exhibited a linear, monotonic association with soil moisture, but there was a non-linear monotonic association between the drought indices and streamflow.