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Flood frequency was estimated by fitting the Pearson type III distribution of both observed and modeled streamflow with historic floods.
With the traditional MK test, 503 rivers had decreased streamflow, with 120 showing significant decreases, whereas 408 rivers had increased streamflow, with 51 showing significant increases.
This study employs the concepts of complex networks to study the temporal dynamics of streamflow, with emphasis on annual scale (i.e., year-to-year connections).
The Correlation of the Baker streamflow with the November April observed Southern Annular Mode (SAM) is significant (1961 2004, r = −0.55, p < 0.001).
This study employed modern concepts of network theory, i.e., complex networks, for studying the temporal dynamics of streamflow, with particular focus on the annual scale, i.e., year-to-year connections.
The comparisons are conducted using 24,000 simulated time series of 110 values, 24,000 simulated time series of 310 values and 92 mean monthly time series of streamflow with varying lengths, as well as 18 metrics.
Similar(41)
The objective of this study was to quantify the variation in estimated relative and absolute changes in streamflow associated with LULC and climate changes with different calibration approaches.
Changes in streamflow predicted with the UC and OC models were compared with those of the SC model.
Phosphorus and nitrogen enrichment are seen as the two most common causes of such eutrophication, with both elements being transported in streamflow and with concentrations strongly dependent upon land-use in the catchment.
Figure 11 indicates that the climate elasticity of streamflow changes with both precipitation and temperature and mainly depends on precipitation.
This procedure can simulate streamflow consistent with observations, but obtained parameters are not optimal.
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