hydrograph explanation and animation
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![Page 1: Hydrograph explanation and animation](https://reader033.vdocuments.mx/reader033/viewer/2022061207/54849a7d5906b5cd158b4797/html5/thumbnails/1.jpg)
Construction
And
Analysis of Hydrographs
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©Microsoft Word clipart
![Page 2: Hydrograph explanation and animation](https://reader033.vdocuments.mx/reader033/viewer/2022061207/54849a7d5906b5cd158b4797/html5/thumbnails/2.jpg)
HydrographRecord of River Discharge (the level of water flowing down a river channel) over a period of time, they show how certain rivers respond to a rainstorm.River Discharge (the level of water flowing down a river) (is calculated)
= cross sectional arearivers mean (average) velocity
X
(at a particular point in its course)
Storm HydrographsShow the change in discharge caused by a period of rainfall
![Page 3: Hydrograph explanation and animation](https://reader033.vdocuments.mx/reader033/viewer/2022061207/54849a7d5906b5cd158b4797/html5/thumbnails/3.jpg)
WhyConstruct & Analyse
Hydrographs ? To find out discharge patterns
ofa particular drainage basin
Help predict flooding events,therefore influence implementation of flood prevention measures
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![Page 4: Hydrograph explanation and animation](https://reader033.vdocuments.mx/reader033/viewer/2022061207/54849a7d5906b5cd158b4797/html5/thumbnails/4.jpg)
Construction
Of Storm (flood) Hydrographs
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![Page 5: Hydrograph explanation and animation](https://reader033.vdocuments.mx/reader033/viewer/2022061207/54849a7d5906b5cd158b4797/html5/thumbnails/5.jpg)
0 12 24 36 48 30 72
Hours from start of rain storm
3
2
1
Dis
charg
e (
m3/s
)
Base flow
Through flow
Overland flowR
isin
g
limb
Recession
limb
Basin lag time
mm4
3
2
Peak flow
Floo
d Hyd
rogr
aph
![Page 6: Hydrograph explanation and animation](https://reader033.vdocuments.mx/reader033/viewer/2022061207/54849a7d5906b5cd158b4797/html5/thumbnails/6.jpg)
0 12 24 36 48 30 72
Hours from start of rain storm
3
2
1
Dis
charg
e (
m3/s
)
The discharge of the river is measured in cumecs - this stands for cubic metres per second
![Page 7: Hydrograph explanation and animation](https://reader033.vdocuments.mx/reader033/viewer/2022061207/54849a7d5906b5cd158b4797/html5/thumbnails/7.jpg)
0 12 24 36 48 30 72
Hours from start of rain storm
3
2
1
Dis
charg
e (
m3/s
)
mm4
3
2
Rainfall shown in
mm, as a bar graph
![Page 8: Hydrograph explanation and animation](https://reader033.vdocuments.mx/reader033/viewer/2022061207/54849a7d5906b5cd158b4797/html5/thumbnails/8.jpg)
0 12 24 36 48 30 72
Hours from start of rain storm
3
2
1
Dis
charg
e (
m3/s
)
mm4
3
2
Discharge in m3/s, as a line graph
![Page 9: Hydrograph explanation and animation](https://reader033.vdocuments.mx/reader033/viewer/2022061207/54849a7d5906b5cd158b4797/html5/thumbnails/9.jpg)
0 12 24 36 48 30 72
Hours from start of rain storm
3
2
1
Dis
charg
e (
m3/s
)
Ris
ing
lim
b
mm4
3
2
Rising limbThe normal
(base) flow of the river
starts to rise when run-off,
ground and soil water
reaches the river.
![Page 10: Hydrograph explanation and animation](https://reader033.vdocuments.mx/reader033/viewer/2022061207/54849a7d5906b5cd158b4797/html5/thumbnails/10.jpg)
0 12 24 36 48 30 72
Hours from start of rain storm
3
2
1
Dis
charg
e (
m3/s
)
Ris
ing
limb
mm4
3
2
Peak flow
Peak flowMaximum
discharge in the river, the time when the
river reaches its
highest flow
![Page 11: Hydrograph explanation and animation](https://reader033.vdocuments.mx/reader033/viewer/2022061207/54849a7d5906b5cd158b4797/html5/thumbnails/11.jpg)
0 12 24 36 48 30 72
Hours from start of rain storm
3
2
1
Dis
charg
e (
m3/s
)
Ris
ing
limb
Recession
limb
mm4
3
2
Peak flow
Recession limbshows that
water is still reaching the river
but in decreasing amounts
![Page 12: Hydrograph explanation and animation](https://reader033.vdocuments.mx/reader033/viewer/2022061207/54849a7d5906b5cd158b4797/html5/thumbnails/12.jpg)
0 12 24 36 48 30 72
Hours from start of rain storm
3
2
1
Dis
charg
e (
m3/s
)
Ris
ing
limb
Recession
limb
Basin lag time
mm4
3
2
Peak flow
Basin lag timeThe time it
takes for the water to find its way to the river
![Page 13: Hydrograph explanation and animation](https://reader033.vdocuments.mx/reader033/viewer/2022061207/54849a7d5906b5cd158b4797/html5/thumbnails/13.jpg)
0 12 24 36 48 30 72
Hours from start of rain storm
3
2
1
Dis
charg
e (
m3/s
)
Base flow
Ris
ing
limb
Recession
limb
Basin lag time
mm4
3
2
Peak flow
Base flowNormal
discharge of the river
![Page 14: Hydrograph explanation and animation](https://reader033.vdocuments.mx/reader033/viewer/2022061207/54849a7d5906b5cd158b4797/html5/thumbnails/14.jpg)
0 12 24 36 48 30 72
Hours from start of rain storm
3
2
1
Dis
charg
e (
m3/s
)
Base flow
Through flow
Overland flowR
isin
g
limb
Recession
limb
Basin lag time
mm4
3
2
Peak flow
Overland flow
Through flow
+
=Storm Flow
![Page 15: Hydrograph explanation and animation](https://reader033.vdocuments.mx/reader033/viewer/2022061207/54849a7d5906b5cd158b4797/html5/thumbnails/15.jpg)
Volume of water
reaching the river from
surface run off
Overland flow
Through flow
Volume of water reaching the
river through the soil and
underlying rock layers
![Page 16: Hydrograph explanation and animation](https://reader033.vdocuments.mx/reader033/viewer/2022061207/54849a7d5906b5cd158b4797/html5/thumbnails/16.jpg)
Analysis
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![Page 17: Hydrograph explanation and animation](https://reader033.vdocuments.mx/reader033/viewer/2022061207/54849a7d5906b5cd158b4797/html5/thumbnails/17.jpg)
Interpretation of Storm Hydrographs
•Rainfall Intensity
•Rising Limb•Recession Limb•Lag time
•Peak flow compared to Base flow•Recovery rate, back to Base flow
You need to refer to:
Basin lag time
0 12 24 36 48 30 72
Hours from start of rain storm
3
2
1
Dis
charg
e (
m3/s
)
Base flow
Through flow
Overland flowR
isin
g
limb
Recession limb
mm
4
3
2
Peak flow
![Page 18: Hydrograph explanation and animation](https://reader033.vdocuments.mx/reader033/viewer/2022061207/54849a7d5906b5cd158b4797/html5/thumbnails/18.jpg)
Some Factors influencing
Storm Hydrographs• Area
• Slope
• Rock Type
• Land Use
• Soil
Precipitation / Temp
©Microsoft Word clipart
![Page 19: Hydrograph explanation and animation](https://reader033.vdocuments.mx/reader033/viewer/2022061207/54849a7d5906b5cd158b4797/html5/thumbnails/19.jpg)
Area
Large basins receive more precipitation than small therefore have larger runoff
Larger size means longer lag time as water has a longer distance to travel to reach the trunk river
Area Rock Type Soil
Slope Land Use Precipitation / Temp
![Page 20: Hydrograph explanation and animation](https://reader033.vdocuments.mx/reader033/viewer/2022061207/54849a7d5906b5cd158b4797/html5/thumbnails/20.jpg)
Slope
Channel flow can be faster down a steep slope therefore steeper rising limb and shorter lag time
Area Rock Type Soil
Slope Land Use Precipitation / Temp
![Page 21: Hydrograph explanation and animation](https://reader033.vdocuments.mx/reader033/viewer/2022061207/54849a7d5906b5cd158b4797/html5/thumbnails/21.jpg)
Rock Type
Permeable rocks mean rapid infiltration and little overland flow therefore shallow rising limb
Area Rock Type Soil
Slope Land Use Precipitation / Temp
![Page 22: Hydrograph explanation and animation](https://reader033.vdocuments.mx/reader033/viewer/2022061207/54849a7d5906b5cd158b4797/html5/thumbnails/22.jpg)
Soil
Infiltration is generally greater on thick soil
The more infiltration occurs the longer the lag time and shallower the rising limb
Area Rock Type Soil
Slope Land Use Precipitation / Temp
![Page 23: Hydrograph explanation and animation](https://reader033.vdocuments.mx/reader033/viewer/2022061207/54849a7d5906b5cd158b4797/html5/thumbnails/23.jpg)
Land Use
Urbanisation - concrete and tarmac form impermeable surfaces, creating a steep rising limb and shortening the time lag
In wooded areas, trees intercept/absorb the precipitation, creating a shallow rising limb and lengthening the time lag
Area Rock Type Soil
Slope Land UsePrecipitation / Temp
![Page 24: Hydrograph explanation and animation](https://reader033.vdocuments.mx/reader033/viewer/2022061207/54849a7d5906b5cd158b4797/html5/thumbnails/24.jpg)
Precipitation & Temperature
Short intense rainstorms can produce rapid overland flow and steep rising limb
If there have been extreme temperatures, the ground can be hard (either baked or frozen) causing rapid surface run off Snow on the ground can act as a store producing a long lag time and shallow rising limb. Once a thaw sets in the rising limb will become steep
Area Rock Type Precipitation / Temp
Soil Slope Land Use
![Page 25: Hydrograph explanation and animation](https://reader033.vdocuments.mx/reader033/viewer/2022061207/54849a7d5906b5cd158b4797/html5/thumbnails/25.jpg)
Remember!
These influencing factors will:
Influence each other
Change throughout the rivers course