rainfall runoff Flashcards
a graph that shows how the flow of water in a river changes over time
hydrograph
it is the normal flow of the water at the river
base flow
the period when the river or stream flow increases due to rainfall
rising limb
highest point on the hydrograph when the rate of discharge is greatest
peak discharge
the time between the peak precipitation and the peak discharge
lag time
when the discharge decreases and the river level falls
falling limb
purpose of hydrograph
-provide information about the contributions of precipitation, soil water, and groundwater to stream runoff, as well as hydrological processes and recharge properties of groundwater during rainfall event
refers to the process of dividing a streamflow hydrograph into its different components
hydrograph separation
this method of baseflow separation is suitable only for individual storm events
straight line method
a method that assumes that base flow declines at a constant rate during and after the storm event and uses fixed time intervals after peak flow to distinguish between base flow and direct runoff
fix base method
a technique used to separate base flow from direct runoff in a streamflow hydrograph that focuses on analyzing the recession limb of the hydrograph after the peak flow. This method assumes that the decline in flow over time is primarily due to base flow, as direct runoff diminishes quickly after the peak
recession curve method
type of hydrographic methods that require hydrologist to perform the method, usually labor intensive and results are subjected to individual hydrologist interpretation
manual method
type of hydrographic methods that utilizes computers in order to eliminate result subjectivity and reduce time required for streamflow record analysis
automated method
represents the direct runoff resulting from 1 cm of effective rainfall over a drainage area
unit hydrograph
assumptions in unit hydrograph
-effective rainfall is uniformly distributed over the entire drainage basin
-the effective rainfall occurs uniformly within its specified duration
-the effective rainfalls of equal duration will produce hydrographs of direct runoff having same or constant time base
-the ordinates of the direct runoff hydrographs having same time base are directly proportional to the total amount of direct runoff given by each hydrograph
-the hydrograph of direct runoff resulting from a given pattern of effective rainfall remain invariable irrespective of its time of occurence