Cumulative frequency curve that shows the percent of time specified discharge was equalled or exceeded during a given period is known as:
flow duration curve
In the study of hydrology and water resources, it is often important to understand how the flow rate, or discharge, of a river or stream varies over time. Different types of graphical representations are used to illustrate these variations for different purposes. The question asks about a specific type of cumulative frequency curve related to discharge.
A cumulative frequency curve that shows the percentage of time a specified discharge was equalled or exceeded during a given period is known as a flow duration curve. This curve is a fundamental tool in hydrology used to characterize the flow variability of a river basin. It plots discharge values on the y-axis and the percentage of time that these discharge values were equalled or exceeded on the x-axis. For example, a point on the curve might show that a discharge of 50 cubic meters per second is equalled or exceeded 30% of the time.
Let's consider why the other options do not fit the description:
Based on the definitions, the only option that matches the description of a cumulative frequency curve showing the percentage of time a specific discharge was equalled or exceeded is the flow duration curve.
The use of unit hydrographs for estimating floods is generally limited to catchments of size less than?
What are the lower and upper limits of catchment area for applicability of the use of unit-hydrograph?
Select the correct option with regard to the following two statements (H1 and H2) pertaining to the hydrograph of a storm in a catchment.
H1: The rising limb of the hydrograph depends on the catchment characteristics only.
H2: The recession limb of the hydrograph depends on the storm characteristics and catchment characteristics.
Basin lag in hydrology is the time difference between the ______.
Isolated storm is represented in a hydrograph with