A stream increases its sinuosity by meandering more in response to a hike in discharge.
The discharge will increase, sinuosity as mentioned above because water is brought into the circulation from tributary streams and groundwater. As discharge will increase, the width, depth, and common velocity of the moving growth. The gradient of the circulate, but, will lower.
In a meandering river, water will tend to flow fastest alongside the out of doors bend of a meander, and slowest at the internal bend. The modifications in land use related to urban improvement have an effect on flooding in lots of approaches. doing away with plants and soil, grading the land floor, and building drainage networks growth runoff to streams from rainfall and snowmelt.
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