Step 1: Understanding the Concept:
A storm hydrograph is a graph showing the rate of flow (discharge) over time at a specific point in a river or channel.
It represents how a catchment basin responds to a rainfall event.
A typical hydrograph consists of a rising limb, a peak segment, and a falling limb (or recession curve).
Step 2: Detailed Explanation:
Let us evaluate both statements:
Statement (I): The rising limb (concentration curve) is the ascending portion of the hydrograph leading up to the peak.
As rainfall continues, water flows over the ground surface and through small channels, gradually filling up storage spaces and reaching the main stream.
This concentration of runoff causes a steady increase in stream discharge, making Statement (I) correct.
Statement (II): The shape of the rising limb is influenced by both the physical properties of the drainage basin and the characteristics of the storm.
Basin characteristics include basin shape, size, slope, drainage density, and soil infiltration capacity.
Storm characteristics include rainfall intensity, duration, and the direction of storm movement.
For example, a circular basin with a steep slope will produce a steep rising limb, while a long, narrow basin will produce a gentler slope.
Thus, both basin and storm characteristics control the shape of the rising limb, making Statement (II) correct.
Consequently, both statements are correct.
Step 3: Final Answer:
Both Statement (I) and Statement (II) are correct.