Option A Freshwater - Drainage Basins Flashcards
Define a drainage basin
Area where all accumulated water supplied by percipitation is transferred to a particular ocean, lake or larger stream.
What is the hydrological cycle
The cycle of water between the biosphere, atmosphere, lithosphere and hydrosphere.
The cycle is seen in drainage basins and can be broken down into inputs, outputs, flows and stores.
What are the inputs and outputs of a drainage basin?
Inputs:
Percipitation
Outputs:
Evaporation
Evapotranspiration
What is evapotranspiration (P.EVT)?
The potential EVT if there was an unlimited supply of water
What are the different flows in a drainage basin?
Infiltration: water soaks into the soil or rock beneath, infiltration capacity is the maximum rate.
Overland flow: flow of water over the land’s surface, occurs when soil is saturated or at infiltration capacity.
Through flow: water flowing through the soil in natural pipes and percolines.
Base flow: part of the river’s discharge provided by groundwater seeping into the bed of a river. Constant, though can increase in wet periods.
What are the different stores in a drainage basin?
Vegetation - water caught and stored by plants
Soil - subsurface water in the soil
Aquifers - permeable rock that acts as an underground reservoir of water
What are the three main components of water stored in vegetation?
Interception: water retained by the plant surface and later evaporated.
Throughfall: water falling through gaps in the vegetation dropping from leaves, twigs or stems.
Stemflow: water that trickles along twigs and branches and finally the main trunk.
Describe the water store of soil.
Soil moisture is the subsurface water in the soil.
Field capacity is the water held in the soil after excess water drains away.
Wilting point defines the point at which plants can no longer take water from the soil.
Explain the processes surrounding aquifers and why they’re important
As water moves from soil to bedrock in percolation, it reaches a permanently saturated zone within the rock, the water table.
The permeability of the rocks dictates how quickly the water gets there.
The water table varies seasonally through the aeration zone. 96.5% of freshwater is from the ground and takes a prolonged period to recycle, hence it is considered non-renewable in certain locations.
The recycling process is known as recharge and occurs by infiltration, seepage, groundwater leakage, and artificial recharge from irrigation.
What is the cryosphere?
The snow and ice environment.
Up to 2/3 of the world’s freshwater is in the form of snow and ice.
What does the Bradshaw model define?
The Bradshaw model approximates changes in the characteristics of a river downstream.
Increase:
Discharge
Occupied Channel Width
Water depth
Water velocity
Load quantity
Decrease:
Load particle size
Channel bed roughness
Slope angle
Summarise water flow in rivers.
HAAS, SSST, laminar, trubulent, cavitation, velocities, meanders, oxbow lakes, waterfalls, rapids.
How are floodplains, meanders, levees, waterfalls and deltas formed?
Waterfalls: Layer of HR over layer of SR. SR erodes faster, forms rapids, plunge pool, undercut, overhanging cliff collapses, retreats, gorge.
Flood plains: Areas of low relief formed by deposition when a river floods. Alluvium is deposited on the land in times of flooding increasing the height of the floodplain.
Meanders: small disruption in channels such as pool, riffle or bend cause imbalanced erosion. Imbalance grows causing a curve. The curve bends further until a thin neck is formed. After continuous flooding, neck breaks, and river straightenes, an oxbow lake is formed.
Levees: deposition of coarse material near the channel while finer deposits are further in the floodplain. Raised banks at the edge of the river. Heavier deposited first due to high energy requirements.
Deltas: When a stream flows into a standing body of water. Loss of energy and a large volume of sediment being deposited. Salty water speeds up process through flocculation.
What is a storm hydrograph and what does each section represent
Show how a river’s discharge changes throughout a particular event.
Rising and recessional limb - rise and fall of discharge.
Peak discharge - highest point on the graph.
Lag time - time between peak rainfall and peak discharge.
Size - Affected by basin, rainfall, geology and surroundings.
Flows - Base flow, through flow, and overground flow.
What influence does geology have on how a river reacts to storms?
Impermeable surfaces generate more overland flow - shorter lag time and higher peak flow.
River regimes?
Influence of seasonality?
River regimes are the seasonal variation in the flow of a river.
Seasonal changes in climate generally have the greatest impact on river flow.
Describe flood risk.
Most river floods are contained within a river’s floodplain.
Larger floods occur less often and cover larger parts of the plain. Increased intensity, decreased frequency.
What factors impact flood risk?
Precipitation type and intensity
Temperature and evapotranspiration
Antecedent moisture
Drainage density
Porosity and impermeability
Slopes
Vegetation type
Land use
What effect does urbanisation have on river flow? How is this seen on a storm hydrograph?
Impermeable surfaces in urbanised spaces cause more surface runoff with drainage channels. This leads to:
- Shorter lag times
- steeper rising limbs
- higher peak flows
- steeper recessional limb#
Magnitude and frequency of floods are increased in at least 3 ways
- Creation of impermeable surfaces
- Smooth surfaces and dense drainage network
- River channels constricted by riverside facilities, roads, bridges
It can have conflicting impacts on hydrological processes:
- More water leading to increased erosion
- Increased speed of flow and material due to enlarged channels
- Less erosion at riverbank protection schemes
Effect of deforestation on river flow
Presence of vegetation increases interception, reduces overland flow and increases evapotranspiration.
Deforestation contrasts each aspect.
- More overland flow leading to more frequent erosion
- River transporting more sediment
- Reduced evapotranspiration
Risk of higher magnitude floods of greater frequency.
Effect of channel modifications on river flow
Include channelisation, enlargement, and straightening. (C,E,S)
C and S form straight channels that speed up the water reducing lag time.
E enables more water flow increasing peak flow.
Purpose is to remove water from an area, works up to a point where severe floods could destroy modifications as in Mississippi and Hurricane Katrina.
What are the 2 types of flood mitigation strategies with examples?
There are hard (dams, channel modification) and soft engineering schemes (planning, afforestation).