Hydrological Cycle Flashcards
Input
Precipitation
Storage
- Interception
- Vegetation storage
- Surface storage
- Groundwater storage
- Channel storage
Flows and Processes
- Surface runoff
- Throughfall (water dripping from leaf to leaf)
- Stemflow (water running down stem)
- Throughflow (downhill through soil)
- Infiltration (soaking into soil)
- Percolation (seeping down into water table)
- Groundwater flow (below water table, through permeable rock)
- Baseflow (groundwater feeding into river)
- Interflow (water flowing above water table in permeable rock)
- Channel flow
Outputs
- Evaporation
- Transpiration
- Evapotranspiration
- River discharge
What is river discharge affected by?
- Precipitation
- Hot weather (rate of evaporation is higher)
- Removal of water
Characteristics of a typical storm hydrograph.
- Peak discharge (highest point on graph)
- Lag time (delay between peak rainfall and peak discharge)
- Rising Limb
- Falling Limb
Physical features that affect lag time and peak discharge.
- Larger drainage basins
- Steep-sided
- Circular basins (because all points on the watershed are roughly the same distance from river thus water flow will reach river at the same time)
- Lots of tributaries
- Human activity (impermeable surfaces and drainage systems)
What does “antecedent moisture” mean?
Amount of water already present.
This means infiltration is reduced and surface run off increases.
Erosion can affect…
the length, depth and width of a river.
Headward erosion
Makes river longer.
Happens near the river’s source as throughflow and surface runoff causes more erosion at the point the water enters the river channel.
Vertical erosion
Makes river deeper.
Upper stages.
Lateral erosion
Makes river wider.
Middle and lower stages of river.
Five man ways in which river erosion happens
- Hydraulic action
- Abrasion (rocks rub against bank and bed_
- Attrition (rocks smash into each other)
- Cavitation (air bubbles in turbulent stretches implode causing shockwaves that break pieces of rock off the bank and beds)
- Solution
Transportation methods
- Solution
- Suspension
- Saltation
- Traction
What is river capacity?
Total load (measured by volume, mass or weight) that a river is able to transport at a particular discharge or energy level. A river's capacity increases as discharge increases.