The higher frequency stream was more salient in piloting and so was attenuated 3 dB so that both streams were of equivalent perceived loudness.
To quantitatively measure landscape features we used several classical geomorphic indices (spacing ratio, hypsometric curves and integral, stream frequency drainage, stream length-gradient).
However, effective integration of high frequency data streams received from permanent sensors remains a challenge.
It is influenced by the length and frequency of streams, geological structures, land use/land cover, climate, relief and slope of the watershed.
Rc was influenced by the length and frequency of streams, geological structures, land use/land cover, climate, relief and slope of the basin.
The circulator ratio is mainly concerned with the length and frequency of streams, geological structures, land use/land cover, climate, relief and slope of the basin.
Circulatory ratio (R c ) is influenced by the length and frequency of streams, geological structures, land use/land cover, climate, relief and slope of the basin.
The circularity ratio (Rc) is influenced by the length and frequency of streams, geological structures, land use/land cover, climate, relief and slope of the basin (Chopra et al. 2005).
The circulatory ratio is mainly focused on the length and frequency of streams, geological structures, land use/land cover, climate, relief, and slope of the basin (Das et al. 2012).
Hence, it is noticed that there is a decrease in stream frequency as the stream order increases and vice versa.
