Water Cycle Flashcards
cryosphere
water held in ice
biosphere
global ecological system with all living beings
blue water
water stored in lakes, streams and groundwater
green water
water stored in soil and vegitiation
precipitation
movement of water in any form
evaporation
change of state of water from liquid and gas
transpiration
diffusion of water from vegetation to the atmosphere
evapotranspiration
combination of evaporation and transpiration
fossil water
ancient deep ground water from fluvial periods
store
reservoirs where water is held such as oceans
flow
movement of water as one part of the system
input
when water enters a source again
output
movement of water out of a source
flux
movement of the rate of flow between stores
what is an example of solar energy?
evaporation and transportation
what is an example of gravitational potential energy?
transformed to kinetic energy
what is the most important flux?
evaporation from oceans
what is evaportation?
water from the ground to the atmosphere
what is the flux of evaporation? number
436.5 km3/year
what is the flux of precipitation?
water from the atmosphere to the ground like rain, snow and hail
what is the flux of precipitation? number
391 km3/year
what is the flux of groundwater runoff?
throughflow like soil and bedrock
what is the flux of groundwater runoff? number
45 km3/year
what is the flux of transpiration?
vegetation to atmosphere to the biosphere
what is the flux of transpiration? number
68.7 km3/year
what are the 6 steps for convectional rainfall?
1 - sun warms earth’s surface
2 - surface warms overlying air
3 - warm air becomes less dense and rises
4 - rising air cools and decreased ability to hold moisutre
5 - cools and reaches saturation and dew point and forms around condensation nuclei
6 - clouds form and it rains and repeats
what are the 4 steps of orographic rainfall?
1 - solar energy heats up the earth’s surface
2 - air rises and reaches condensation and nuclei and forms around condensation nuclei
3 - rains on the stoff side of the mountian
4 - dry decending air fall of lee side of the mountains
what are the 4 steps of frontal rainfall?
1 - solar energy heats up surface layer
2 - cool air block causes warm air to rise
3 - air reaches saturation and dew point and forms around condensation nuclei
4 - air condensed into clouds and process repeats
what is an example of convectional rainfall?
amazon
what is an example of orographic rainfall?
Himalyays
what is an example of frontal rainfall?
UK
what is a meterlogical drought?
deficit in precipitation
what is a agricultral drought?
deficit in soil moisutre
what is a hydrological drought?
deficit in all stores
what is a famine drought?
widespread crop failure
El Nino year causing drought in Australia
- Westward trade winds reverse so cold water off coast of Peru replaced by warm water and warm water off coast of Australia replaced by cold water
- Rising ocean temps. creates convectional rainfall on coast of Peru, creating wetter conditions
- Dry air returns to Australia so less precipitation which leads to meteorological drought
La Niña
unusually cold sea surface
temperatures found in the eastern
tropical Pacific. A La Niña episode
may follow an El Niño.
what is a river regime?
measure of annual variationa in river with discharge measured in cumecs
where is the Yukon river located?
Canada
what influences the Yukon river regime in Canada?
- precipitation falls as snow
- locked in cryopshere and melts in June
- increases river discharge and into winter it freezes again
where is the Indus river located?
Himalayas
what influences the Indus river regime in the Himalayas?
- snow melt hits peak discharge in May
- June 4 month monsoon season with North shift of ITCZ
- august dry season starts
- global warming = less snow melt due to increased evaporation
what influences river regimes in the Amazon river?
- large convectional rainfall
- june peak discharge is created and takes 4 months for the tributries to catch up with the river
- winter = decreased rainfall
how long are the tributaries in the Amazon river?
2,900,000 sq meters
how can overlying soil influence river regimes?
influences time for inputs to reach the river
how can sandy soil influence river regimes?
allows infiltration to occur as it is more permeable
what are the 2 types of storm hydrographs?
flashy
delayed
what are 4 features of a FLASHY storm hydrography?
1 - steeper rising limb
2 - higher peak discharge
3 - gradual falling limb
4 - shorter time to exceed bank full discharge
what are 4 features of a DELAYED storm hydrograph?
1 - slower rising limb
2 - lower peak discharge
3 - steeper falling limb
4 -longer time to exceed bank full discharge
what are the 7 physical factors influencing storm hydrographs?
1 - climate
2 - relief and gradient
3 - overlying soils and geology
4 - vegetation
5 - size
6 - shape
7 - density
how does climate affect storm hydrographs? 5 rain
- intense rainfall over extended period of time
- soils become saturated
- less infiltration and percolation
- less throughflow and ground water flow
- increased water travelling by overland flow -> flood
how does relief and gradient affect storm hydrographs? 3
- steep gradient and relief = increased gravitational potential energy
- increase in overland flow
-> flood
how does overlying soils and geology affect storm hydrographs? 4
- if overlying soils is impermeable will decrease infiltration and overland flow
- if geology consists on non-pourus rock water cannot percolate
- increased saturation in the soil layer
- decreased infiltration -> flood
how does vegetation affect storm hydrographs? 4
- if there was a decrease in veg density there would be a decrease in interception
- decreased evapotranspiration
- increased like hood of ground being saturated and overland flow occurring
- increase the amount of water hitting the ground directly so increased soil compaction so increased overland flow
how does size affect storm hydrographs? 2
- smaller drainage basins produce more FLASHY hydrographs
- water has a shorter distance to travel to the channel flow so there would be a steeper rising limb and lag time
how does density affect storm hydrographs? 2
- is there are more tributaries it is more likely to be a FLASHY hydrograph as the flow is faster and it is more likely to make the water arrive at similar times
- increase flood etc
how can deforestation affect storm hydrographs? 4 - increase flood risk
- leads to decreased interception and evapotranspiration
- 25% of water returned to atmosphere in a healthy forest
- increase water on soil
- soils become saturated -> increased overland flow -> flood
how can deforestation in relation to decreased stem flow and throughfall affect storm hydrographs? 3 - increase flood risk
- less of a delay in water hitting the ground
- infiltration rates are less likely to cope with levels of water
- increased saturated overland flow -> flood
how can an increase in soil compaction from deforestation affect storm hydrographs? 5 - increase flood risk
- more water hitting the ground directly
- amazon had had 17% of it deforested
- convectional rainfall causes soil compaction
- less infiltration so increased OVERLAND FLOW -> flood
overtime the soil has less nutrients and so decreased ability to grow back
how can urbanisation affect storm hydrographs? - increase flood risk
- leads to an increase in areas with paved impermeable surfaces
- infiltration is not happening meaning an increase in overland flow
- paved areas provide low friction routes to drains to the river channel
- increase the levels of water hitting the ground at the same time
- increase overland flow -> flood
how can man made structures at the river increase flood risk?
- increased rainfall so increased debris in the water
- urbanised areas have river management strategies
- to increase channel flow to keep up with drainage
- eg levees have raised banks to increase the amount that the river can hold
- if flood waters rise -> water stays in place longer as debris is trapped in the river
what is a water budget?
balance between inputs and outputs
what is a surplus?
saturated soils
what is a defecit?
vegetation depleting the soil store
what is a recharge?
it follows a deficit and is where infiltration occurs
what is utilisation?
follows a surplus where vegetation uses moisture