The first step in morphometric analysis of a drainage basin is the designation of stream order; stream ordering as suggested by Strahler (1964) was used for this study.
Stream ordering is defined as a measure of the position of a stream in the hierarchy of tributaries (Leopold et al. 1964) and the streams of Shanur River Basin have been demarcated according to the Strahler's system of stream ordering.
The first step in the geomorphological analysis of a drainage basin is the designation of stream order; stream ordering as suggested by Strahler (1964) was used for this study.
In this paper, we show that the per-stream ordered SNR converges asymptotically (with delay spread) to the inverse, marginal cumulative distribution function (CDF) of post-processing SNR.
Stream ordering is an interesting concept.
Giant salamander detection probability was positively associated with stream temperature regardless of stream order, and was higher in second- and third-order streams than first-order streams.
Overall, deposition rates increase with decreasing stream order, reflecting greater hillslope/channel coupling in low-order streams.
The nature of vegetation clearing was characterised based on land tenure, slope and stream order.
Changes in stream order produced exponential changes in the total number, mean segment length and total length of streams.
Maximum stream temperature (Tmax) is mainly controlled by base flow index, percent forest land cover, and stream order.
We adapted the stream order analysis technique to examine the changes in tidal channel morphology within marsh restoration projects.
