water cycle Flashcards
precipitation
all forms of moisture that reach the Earth’s surface
Groundwater flow
the deeper movement of water through underlying permeable rock below the water table
surface runoff/overland flow
the movement of water over the surface of the land, usually when the ground is saturated or frozen when precipitation is too intense for infiltration to occur
percolation
the gravity flow of water within the soil
evaporation
the transformation of water droplets into water vapour by heating
evapotraspiration
the combine effects of transpiration and evaporation-loss of water from ground surfaces and vegetation into the atmosphere
condensation
water vapour in the air is changed to liquid water
infiltration
the downward movement of water into the soil surface
sublimation
the process of snow and ice changing into water vapour in the air without first melting into water
advection
the movement of water through the atmosphere
global water budget
the annual balance of fluxes and the size of water store. the constant circulation of water within the cycle means that water is considered a renewable resource
stores
reservoirs where water is held
fluxes
the rate of flow between stores
processes
the physical mechanisms that drive the fluxes between the stores
inputs
precipitation
stores
interception, vegetation, surface, soil moisture, groundwater, channel
flows and processes
infiltration, through flow, percolation, stem flow, base flow, channel flow, surface runoff
outputs
evaporation, transpiration, evapotranspiration, river discharge
interception
temporary storage as water is captured by plants, buildings and hard surfaces before reaching the soil
vegetation
any moisture taken up by vegetation and held within plants
surface
any surface water in lakes, ponds, puddles
soil moisture
water held within the soil
groundwater storage
water held within permeable rocks
channel storage
water held in rivers and streams
infiltration
water entering the topsoil.
throughflow
water seeping laterally through soil below the surface, but above the water table
percolation
the downward seepage of water through rock under gravity, especially on permeable rock
stem flow
water flowing down plant stems or drainpipes
base flow
also known as groundwater flow. slow-moving water that seeps into a river channel
surface runoff
flow over the surface during an intense storm, or when the ground is frozen, saturated or on impermeable clay.
evaporation
the conversion of water to vapour
transpiration
water taken up by plants and transpired onto the leaf surface
evapotranspiration
the combined effect of evaporation and transpiration
river discharge
the volume of water passing a certain point in the channel over a certain amount of time.
what are the three types of rainfall?
orographic, convectional, frontal
orographic rainfall
the western side of the UK receives the highest rainfall totals, especially in autumn and winter. warmer moist Atlantic air from the south-west is forced to rise as it reaches the western uplands. as it rises, it cools over the high ground-producing heavy rain over western and northern parts of the UK
Convectional rainfall
this is typical of the eastern and south-eastern UK in summer, during periods of high temperatures. The rainfall created is often intense and associated with electrical storms and thunder
frontal rainfall
brings the most rainfall to the UK over the course of a year. fronts are formed as part of a low-pressure area when warmer moist air from the south-west meets colder Polar air from the north or north-west. the warmer air is forced to rise over the denser colder air-forming rain along both warm and cold fronts
weather fronts
transition zone between two contrasting bodies of air. the front is where they meet that have different temperatures and humidity where the reaction as the masses meet brings a dramatic change in weather conditions. the larger the difference, the more intense the weather is.
china- hard engineering schemes
water transfer scheme that diverts 44.8 billion litres of water from Yangtze in the South to Yellow Basin in the North.
benefits: saved china from water conflict and provides fair water distribution.
consequences: displaced 345,000 villagers, exacerbates water pollution.
megadams (HE)
there are 57,000 global mega dams
kariba Dam on Zambezi was a huge economic development plan in 1950.
however: 57,000 people were displaced by dam and they are still in poverty and famine.
desalination (HE)
sustainable process to conserve supplies for future generations. draws from ocean supplies. TNCs are building desalination plants around the world (Veolia, Salina Impregilo) with growing desalination locations e.g. USA, UAE, Spain, Kuwait.
Sustainable water management: water conservation
NGOs (Farm Africa, WaterAid) are used to develop a range of strategies to combat climate change through water conservation. for example, farmers are trained in minimising tilling which absorbs rainwater and limits evaporation to conserve water.