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what is a drainage basin
areas of land where water from rain or snow melt drains downhill into a body of water like a river, lake or ocean.
what are the features of a drainage basin
watershed
source
tributary
confluence
floodplain
mouth
what is a watershed
the boundary between drainage basin, the peak of hills/mountains
what is a source
the beginning of a river, in upland areas
what is a tributary
a smaller river which joins up to a larger river
what is a confluence
the join of two rivers
what is a floodplain
the flat land either side of a river, larger in the lower course of a river
what is a mouth
the end of a river, usually flowing into a lake, the sea or an ocean
what is an open system
allows energy and matter to exchange
what is a closed system
only allow for energy transfer within the system
what is the only input in a drainage basin system?
precipitation
what is the above ground transfers/flows in a drainage basin
throughfall
stemflow
overland flow
channel flow
what are the below ground flows/transfers in a drainage basin system
infiltration
percolation
throughflow
groundwater
base flow
what are the above ground stores in a drainage basin system
interception
surface water
channel storage
what are the underground stores in a drainage basin system
soil water
groundwater
water tables
recharge
springs
what are the outputs in a drainage basin system
evaporation
evapotranspiration
river discharge
what is precipitation and is it an Input, Output or Store
any moisture from a cloud which falls in the drainage basin
(Input)
what is throughfall and is it an Input, Output or Store
any precipitation dripping off branches and leaves to the ground after interception
(Above ground Transfer/Flow)
what is stem flow and is it an Input, Output or Store
any precipitation running down plant stems, trunks after interception
(above ground transfer)
what is overland flow and is it an Input, Output or Store
any precipitation flowing over the ground surface towards a river or other body of water
(transfer above ground)
what is channel flow and is it an Input, Transfer, Output or Store
water flowing within the river channel
(Above ground tranfer)
what is infiltration and is it an Input, Transfer,Output or Store
the process by which water is absorbed by soil. in a downward movement from the surface
(below ground transfer)
what is perolocation and is it an Input, Transfer,Output or Store
the downward movement of water through the soil and bedrock after infiltration has taken place
what is throughflow and is it an Input, Transfer,Output or Store
water moving through the soil under gravity towards the stream
(Transfer below ground)
what is groundwater and is it an Input, Transfer,Output or Store
water moving through the rock under gravity towards the stream
(underground transfer)
what is base flow and is it an Input, Transfer,Output or Store
the lateral movement of water in the bedrock which discharges into a stream from ground water store
(underground transfer)
what is interception and is it an Input, Transfer,Output or Store
the trapping of water during rain on leaves of vegetation preventing it from initially reaching the ground
(stores)
what is surface water and is it an Input, Transfer,Output or Store
water stored on the ground surface in lakes, puddles or ice
(store)
what is channel storage and is it an Input, Transfer,Output or Store
water held within the river channel itself (store)
wha is soil water and is it an Input, Transfer,Output or Store
water from rain is stored in the soil pores after infiltration (store)
what is groundwater and is it an Input, Transfer,Output or Store
water is stored in the permeable rocks after perolocation beneath the water table
what is the water table
the upper surface of the saturated zone, where all soil and rock pores are full with water
what is recharge
the process when water is added to the groundwater store via rain infiltration, percolation
what is evaporation and is it an Input, Transfer,Output or Store
water changes phase from a liquid to a gas with the addition of heat (output)
what is evapotranspiration and is it an Input, Transfer,Output or Store
the combined total of evaporation and transpiration where water moves from soil and plants surfaces in the atmosphere (output)
what is transpiration
biological process where water is released as vapour through stomata in leaves
what are the two types of evapotranspiration
potential evapotranspiration (PET)
Actual evapotranspiration (AET)
what is PET (potential evapotranspiration)
the amount of Evapotranspiration that would occur if there was unlimited water supply
High in hot dry regions due to intense solar radiation
what is AET (Actual evapotranspiration)
the real amount of Evapotranspiration, often lower than PET because of limited soil moisture
what are storm hydrographs
a type of graph that shows how the discharge changes overtime in response to a rainfall event
what is river discharge
amount of water flowing in a river
what are the key components of a storm hydrograph
time on the x axis (usually in hours)
river discharge on the y - axis (measured in cumecs)
rainfall shown as a bar chart
baseflow
rising limb
peak discharge/flow
lag time
falling limb
what does the rising limb of a hydrograph represent?
the steep part of the graph where discharge increases rapidly after rainfall
what is the lag time
the time between peak rainfall and peak discharge
what is the baseflow
the normal day to day discharge of the river before and after rain
what is peak discharge/flow
occurs when the river reaches its highest level
what is the falling limb represent
when discharge decreases and river levels fall. it has a gentler gradient than the rising limb
is a hydrograph is flashy what are the characteristics and where is it located
steep rising limb and short lag time
likely in urban areas
if a hydrograph is gentler, what are the characteristics and where is it located
gentle rising limb and longer lag time
likely in rural areas where is there lots of vegetation
what are some factors which affect a storm hydrograph
climate, and drainage basin characteristics like size, shape, density, soil and rock type, slopes, and vegetation and land use
what are some ways the climate influences the storm hydrograph
torrential rain produces overland flow, a steep rising limp and high peak flow
low intensity rainfall produces infiltration, a gentle rising limb and low peak flow
high temps cause more evaporation so river discharge decreases
dense vegetation cover intercepts more rainfall and leads to less river discharge
saturated ground leads to a steep rising limb and high peak flow
what are some ways drainage basins influences the storm hydrograph
smaller drainage basins produce a steep rising limb and high peak flow
circular drainage basins respond quickly to rainfall than linear basins
impermeable rocks slow down infiltration and percolation
steeper slopes slow down infiltration and speed up surface runoff
whats an annual hydrograph show
how a rivers discharge changes over the course of a year, rather than just during one rainfall event. it reflects seasonal patterns in climate, vegetation, and human activity that influence river flow.
what is the other name of annual hydrographs
river regime
what are the key features of an annual hydrograph?
peak flow - month with the highest discharge
low flow - month with the lowest discharge
what are all the factors that influence annual hydrographs
climate and precipitation
temp
vegetation
soil and geology
human activity
snowmelt rivers
monsoonal rivers
how does climate and precipitation affect annual hydrography
rivers in temperate climates may peak in winter (more rain, Low ET) Monsoonal regions have one strong wet season peak. Glacial Rivers peak in summer due to snow/ice melt
how does temperature influence annual hydrographs
high summer temps - High ET
lower discharge in some rivers.
Cold winters - snow storage
with a sudden melt peak in spring
how does vegetation affect annual hydrographs
dense vegetation intercepts rainfall and increases ET, reducing discharge during growing seasons.
how does soil and geology affect annual hydrographs
permeable soils even out flow; impermeable geology causes flashy seasonal variations
how does human activity affect annual hydrograph
dams, irrigation and water use flatten or alter natural seasonal patterns
how does snowmelt rivers affect annual hydrograph
low flows in winter when precipitation in locked as snow, sharp rise in spring melt.
how do monsoonal rivers affect annual hydrograph
distinct high flow in monsoon season prolonged low flows in dry season
what are some examples of factors affecting annual hydrographs in NZ
Waikato river:
more even flow year-round because of lakes and reservoirs flattening seasonal variation.
list some short facts about the waikato river case study
Longest River in NZ - 425km
Source:: Ruapehu (2797m)
Dams: Waipapa, Arapuni
what is the Abbreviation for Erosion
A . A. S. H
Abrasion
Attrition
Solution
Hydraulic Action and Cavitation
what is abrasion
the rivers load is thrown against the bed and banks scraping them away like sand paper
major process of channel widening and deepening
common in steep river areas
what is attrition
particles carried by the river collide with each other breaking down into smaller, rounder smoother pieces
doesn’t erode the river channel itself but reduces sediment size
what is solution
soluble minerals (e.g limestone) are dissolved by acidic water and carried away in solution.
most effective in rivers flowing through chalk
chemical process rather than physical
what is HA and cavitation
the force of fast flowing water hitting the riverbank and bed. compresses air in cracks, causing rock to weaken and break apart
what are some factors affecting erosion
deforestation
bed load
ph level
agriculture
river engineering
climate change
channel shape
discharge
vegetation
climate and weather
does the upper course experience more lateral or vertical erosion
vertical
does the lower course experience more lateral or vertical erosion
lateral
what is the global sediment yield
the amount of sediment (soil, sand, rock and shingle) transported from land to oceans by rivers per year, usually measured in tonnes per kilometre per year
what types of regions usually have high sediment yields
mountainous, tectonically active regions (Himalayans, Andes mountains)
Deforestes tropical basins (Amazon)
what types of regions usually have low sediment yields
flat, heavily vegetated basins (Amazon Floodplains)
cold stable landscapes with permafrost (Siberia)
what are factors influencing sediment yields
Relief
Climate
Rock type
Vegetation Cover
Drainage Basin Size
Human Activity
Glaciation
how does relief affect sediment yields
steeper mountain rivers, (Himalayans, Andes) have high energy flows, eroding quickly and producing huge sediment yields
how does climate affect sediment yields
heavy rainfall - high runoff and erosion
arid climates have flashy flows causing bursts of erosion
how does rock type affect sediment yields
soft rocks and soils produce higher yields than resistant rocks
what is the waikato’s global sediment yield
50-100 t/km squared per year as although there is volcanic soil, lots of dams trap the sediment in the upper course and prevent it from being transported downstream.
what is the Acronym for Transportation
TSSS
traction
saltation
suspension
solution
what is Traction
heaviest material is rolled along the river bed this requires the most energy.
what is saltation
sand sized particles are bounced along the riverbed in a leap-frog motion
what is suspension
small particles are carried within the water by turbulent flow
what are factors affecting the amount of material that a river can transport
discharge - increase discharge = more transportation
velocity - increased speed = more transportation
what is capacity
the largest amount of load that a stream/river can carry
the greater the discharge, the higher the capacity
the greater the velocity the higher the capacity
what is competence
the diameter of the largest particle that can be carried
the greater the velocity the higher the competence
what is deposition
when a river loses energy and drops the load its carrying, ususlaly largest and coursest material first, then smaller finer material
what is the smallest material and what is the largest
smallest: clay
largest: boulders
what are the main causes of deposition?
decrease in velocity
decrease in discharge
channel widening or gradient decrease
obstructions
meeting still water
how does a decrease in velocity cause deposition
slower flow reduces the rivers ability to transport material
e.g) inside bends of meanders
how does decrease in discharge cause deposition?
less water means less energy to carry load
how does channel widening and gradient decrease cause deposition
rivers spread out and lose energy
how does obstructions cause deposition
natural/ man-made features slow water like dams
what does the hjulstrom curve show
the relationship between a rivers velocity and its ability to erode, transport or deposit sediment of different sizes.
what are the three key terms relating to channel flow
Velocity
Discharge
Thalweg
what is velocity?
the speed at which water moves through a river channel measured in metres per second (m/s)
what are some key points about velocity?
slower near banks and beds due to friction
influenced by channel gradient, roughness, width depth etc..
velocity is not uniform: fastest flow is slightly below the surface and follows the thalweg
finish the sentence about velocity: the higher the gradient…..
the faster the river flow