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Construction And Analysis of Hydrographs © Microsoft Word clipart © Microsoft Word clipart
Hydrograph Record 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) Storm Hydrographs Show the change in discharge caused by a period of rainfall =  cross sectional area rivers mean (average) velocity X (at a particular point in its course)
Why Construct & Analyse Hydrographs ? ,[object Object],[object Object],[object Object],[object Object],© Microsoft Word clipart
Construction Of  Storm (flood) Hydrographs © Microsoft Word clipart
0  12  24  36  48  30  72 Hours from start of rain storm 3 2 1 Discharge (m 3 /s) Base flow Through flow Overland flow Rising limb Recession limb Basin lag time mm 4 3 2 Peak flow Flood Hydrograph
The discharge of the river is measured in  cumecs  - this stands for cubic metres per second 0  12  24  36  48  30  72 Hours from start of rain storm 3 2 1 Discharge (m 3 /s)
0  12  24  36  48  30  72 Hours from start of rain storm 3 2 1 Discharge (m 3 /s) mm 4 3 2 Rainfall shown in mm, as a bar graph
0  12  24  36  48  30  72 Hours from start of rain storm 3 2 1 Discharge (m 3 /s) mm 4 3 2 Discharge in m 3 /s, as a line graph
0  12  24  36  48  30  72 Hours from start of rain storm 3 2 1 Discharge (m 3 /s) Rising limb mm 4 3 2 Rising limb The normal (base) flow of the river starts to rise when run-off, ground and soil water reaches the river.
0  12  24  36  48  30  72 Hours from start of rain storm 3 2 1 Discharge (m 3 /s) Rising limb mm 4 3 2 Peak flow Peak flow Maximum discharge in the river, the  time when the river reaches its highest flow
0  12  24  36  48  30  72 Hours from start of rain storm 3 2 1 Discharge (m 3 /s) Rising limb Recession limb mm 4 3 2 Peak flow Recession limb shows that water is still reaching the river but in decreasing amounts
0  12  24  36  48  30  72 Hours from start of rain storm 3 2 1 Discharge (m 3 /s) Rising limb Recession limb Basin lag time mm 4 3 2 Peak flow Basin lag time The time it takes for the water to find its way to the river
0  12  24  36  48  30  72 Hours from start of rain storm 3 2 1 Discharge (m 3 /s) Base flow Rising limb Recession limb Basin lag time mm 4 3 2 Peak flow Base flow Normal discharge of the river
0  12  24  36  48  30  72 Hours from start of rain storm 3 2 1 Discharge (m 3 /s) Base flow Through flow Overland flow Rising limb Recession limb Basin lag time mm 4 3 2 Peak flow Overland flow Through flow + = Storm Flow
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
Analysis © Microsoft Word clipart
Interpretation of Storm Hydrographs ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],You need to refer to: Basin lag time 0  12  24  36  48  30  72 Hours from start of rain storm 3 2 1 Discharge (m 3 /s) Rising limb Recession limb mm 4 3 2 Peak flow Base flow Through flow Overland flow
Some Factors influencing Storm Hydrographs ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],© Microsoft Word clipart
Area ,[object Object],[object Object],Area Rock Type Soil Slope Land Use  Precipitation / Temp
Slope ,[object Object],Area Rock Type Soil Slope Land Use  Precipitation / Temp
Rock Type ,[object Object],Area Rock Type Soil Slope Land Use   Precipitation / Temp
Soil ,[object Object],[object Object],Area Rock Type   Soil Slope Land Use  Precipitation / Temp
Land Use ,[object Object],[object Object],Area Rock Type Soil Slope Land Use Precipitation / Temp
Precipitation & Temperature ,[object Object],[object Object],[object Object],Area Rock Type   Precipitation / Temp Soil Slope   Land Use
Remember! These  influencing factors  will: ,[object Object],[object Object]

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Hydrograph explanation and animation

  • 1. Construction And Analysis of Hydrographs © Microsoft Word clipart © Microsoft Word clipart
  • 2. Hydrograph Record 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) Storm Hydrographs Show the change in discharge caused by a period of rainfall = cross sectional area rivers mean (average) velocity X (at a particular point in its course)
  • 3.
  • 4. Construction Of Storm (flood) Hydrographs © Microsoft Word clipart
  • 5. 0 12 24 36 48 30 72 Hours from start of rain storm 3 2 1 Discharge (m 3 /s) Base flow Through flow Overland flow Rising limb Recession limb Basin lag time mm 4 3 2 Peak flow Flood Hydrograph
  • 6. The discharge of the river is measured in cumecs - this stands for cubic metres per second 0 12 24 36 48 30 72 Hours from start of rain storm 3 2 1 Discharge (m 3 /s)
  • 7. 0 12 24 36 48 30 72 Hours from start of rain storm 3 2 1 Discharge (m 3 /s) mm 4 3 2 Rainfall shown in mm, as a bar graph
  • 8. 0 12 24 36 48 30 72 Hours from start of rain storm 3 2 1 Discharge (m 3 /s) mm 4 3 2 Discharge in m 3 /s, as a line graph
  • 9. 0 12 24 36 48 30 72 Hours from start of rain storm 3 2 1 Discharge (m 3 /s) Rising limb mm 4 3 2 Rising limb The normal (base) flow of the river starts to rise when run-off, ground and soil water reaches the river.
  • 10. 0 12 24 36 48 30 72 Hours from start of rain storm 3 2 1 Discharge (m 3 /s) Rising limb mm 4 3 2 Peak flow Peak flow Maximum discharge in the river, the time when the river reaches its highest flow
  • 11. 0 12 24 36 48 30 72 Hours from start of rain storm 3 2 1 Discharge (m 3 /s) Rising limb Recession limb mm 4 3 2 Peak flow Recession limb shows that water is still reaching the river but in decreasing amounts
  • 12. 0 12 24 36 48 30 72 Hours from start of rain storm 3 2 1 Discharge (m 3 /s) Rising limb Recession limb Basin lag time mm 4 3 2 Peak flow Basin lag time The time it takes for the water to find its way to the river
  • 13. 0 12 24 36 48 30 72 Hours from start of rain storm 3 2 1 Discharge (m 3 /s) Base flow Rising limb Recession limb Basin lag time mm 4 3 2 Peak flow Base flow Normal discharge of the river
  • 14. 0 12 24 36 48 30 72 Hours from start of rain storm 3 2 1 Discharge (m 3 /s) Base flow Through flow Overland flow Rising limb Recession limb Basin lag time mm 4 3 2 Peak flow Overland flow Through flow + = Storm Flow
  • 15. 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
  • 16. Analysis © Microsoft Word clipart
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