·
Hydrograph
represent the relation between instantaneous discharge and time at a given
point on the stream.
·
It
shows integrated effect of physiographic and meteorological condition on runoff
(discharge) from a catchment.
Components of Hydrograph
·
·
Uses of Hydrograph
§ In flood damage mitigation
by structural and non-structural measures.
§ In flood forecasting.
§ In design of hydraulic
structures like dam, spillway, water convey structure etc.
Hydrograph
depends:
·
Meteorological
factors :-
§ Areal distribution or
rainfall over the basin
§ Size and duration of the
storm event
·
Physiographic
or watershed factors :-
§ Size and shape of the
drainage area
§ Slope of the land surface
and channel
§ Channel morphology and
drainage type
§ Soil types and distribution
§ Storage detention in the
watershed
§ land use and land cover
Factor affecting shape of hydrograph
·
The Drainage Basin
·
Shape of the
drainage basin
·
It influences the time taken by water
to reach the outlet from farthest point and hence affect the time after which
peak discharge attained.
·
Basin A will yield peak discharge
early because most of the point are near to the basin outlet.
·
Basin B will have late peak
discharge, because point are far away from outlet of basin.
·
Basin C will have two peak discharge,
also called complex hydrograph.
·
For a circular drainage basin, the
river’s hydrograph have a steep rising limb, symmetrical and high peak
discharge.
·
Reason- in this type of
basin all point in drainage basin are at equal distance from river or stream so
water can take equal travel time to reach the river.
·
Some other factor based on shape are
as follows:
1. Form factor: it is the ratio
of average width of the basin to the axial length.
2. Compactness Coefficient: it is the ratio
of perimeter of the basin to the perimeter of a circle, whose area is same as
that of the basin.
Compactness
Coefficient: P/(2*pie)
For
circular basin value =1
·
Stream density
·
This is defined as the no. of streams
per unit area of the catchment area. If value of stream density is more peak
discharge will happen early.
·
Drainage density
·
This is defined as the total length
of stream per unit area of the catchment. If value of stream density is more
peak discharge will happen early.
·
The size of the
drainage basin
·
Large size basin catch more water
compare to small size basin so hydrograph resulting from large size basin have
high peak compare to small size basin.
·
Hydrograph resulting from small size
basin have shorter leg time compare to large size basin.
Reason- in small size
basin water can take less time to reach river or basin.
QP= k. An
K= constant, A= Area of catchment, QP= Peak
discharge
·
Basins slopes
·
Basin having Steep slope give high
peak discharge and a short lag time hydrograph.
Reason- water take less
travel time on steep steep slope.
·
Non-porous and impervious rocks responsible
for high peak discharge and shorter lag time.
·
Rainfall intensity
·
More rainwater results in more water
in the river or in other word higher discharge. So higher intensity storm or
rainfall responsible for higher peak discharge and shorter lag time
·
Effect of wind
·
Direction of wind’
·
Soil moisture condition
·
Land use and land cover