Topic 5: The Water Cycle and Water Insecurity Flashcards
closed system
inputs = outputs, there are no inputs or outputs of matter from an external source
solar energy
energy from the sun, heating water and causing evaporation/transpiration
gravitational potential energy
ways in which water accelerates under gravity, thus transporting it to rivers and eventually to the sea
precipitation
input
moisture in any form, e.g. rain, snow, sleet and hail
interception
storage
temporary storage, as water is captured by plants, buildings and hard surfaces before reaching the soil
vegetation storage
storage
any moisture taken up by vegetation and held within plants
surface storage
storage
any surface water in lakes, ponds and puddles
soil moisture
storage
water held within the soil
groundwater storage
storage
water held within permeable rocks (also known as an aquifer)
channel storage
storage
water held in rivers and streams
infiltration
flow
water entering the topsoil, most common during slow or steady rainfall
throughflow
flow
water seeping laterally through soil below the surface, but above the water table
percolation
flow
the downward seepage of water through rock under gravity, especially in permeable rocks e.g. sandstone and chalk
stem flow
flow
water flowing down plant stems or drainpipes
groundwater flow
flow
slow-moving water that seeps into a river channel through rocks
channel flow
flow
the volume of water flowing within a river channel
surface runoff
flow
flow over the surface during an intense storm, or when the ground is frozen, saturated or impermeable
evaporation
output
the conversion of water to vapour
transpiration
output
water taken up by plants and transpired from the leaf surface
evapotranspiration
output
the combined effect of evaporation and transpiration
river discharge
output
the volume of water passing a certain point in the channel over a certain amount of time
potential evapotranspiration (PE)
an estimate of the amount of water lost through evaporation and transpiration in any given period, depending on temperature and air humidity
positive feedback
when a change leads to a decrease within a system and creates instability
negative feedback
when a change tends to reinforce a system, leading to stability
tipping point
when a system changes from one state to another, irretrievably
resilience
the ability of a system to ‘bounce back’ and survive
Walker Cell
the circulation of air whereby upper atmospheric air moves eastwards, and surface air moves west across the Pacific, causing trade winds
water scarcity
an imbalance between demand and supply of water
physical scarcity
insufficient water to meet demand
economic scarcity
people cannot afford water, even when it’s available
water stress
if a country’s water consumption exceeds 10% of its renewable freshwater supply, including difficulties in obtaining new quantities of water, as well as poor water quality restricting usage
water insecurity
the state where present and future supplies of water cannot be guaranteed, caused by water scarcity and water stress
virtual water
water transferred by trading in crops and services that require large amounts of water for their production
aquifer
an underground reservoir most commonly formed in rocks such as chalk and sandstone
convectional rainfall
when the ground warms up, evaporation takes place and the air above is heated and rises - the rainfall created is often intense and associated with electrical storms and thunder
cryosphere
the frozen part of the Earth’s hydrological system
flux
refers to the movement or transfer of water between stores
frontal rainfall
formed when warmer moist air meets colder Polar air - the warmer air is forced to rise over the denser colder air, creating low-pressure and rain
Inter-Tropical Convergence Zone (ITCZ)
a narrow zone of low pressure near the Equator where northern and southern air masses converge
orographic rainfall
when warm, moist air is forced to rise over upland areas, causing the moisture to condense and create rainfall
rain-shadow effect
when orographic rainfall has occurred over an upland area, the area on the lee side of the hills will receive less rain because the air descends, warms and becomes drier
store
an accumulation or quantity of water in a system
thermohaline circulation
the flow of warm and cold water that circulates around the world’s oceans
water budget
the difference between inputs of water (e.g. precipitation) and outputs of water (e.g. evapotranspiration) in any given area