Topic 5: The Water Cycle and Water Insecurity COPY Flashcards
what type of system is the hydrological cycle?
it is a closed system meaning it is finite and constant. it includes includes stores and transfers.
what is the hydrological cycle driven by?
it is driven by solar energy and gravitational potential energy.
1) solar energy- has water and turns from a liquid to a gas, rises into the atmosphere and cools and condenses to form clouds
2) gravitational potential- earth’s gravity pull is converted into kinetic energy and accelerates water through the cycle (falling as precipitation, flowing across the land, infiltrating and percolating)
what is the cryosphere and biosphere?
cryosphere- the ice system (ice sheets and glaciers)
biosphere- the living system (plants and animals)
what is a residence time?
how long water stays in a particular store
what is fossil water?
water that is no longer being naturally replenished. it may have been stored for a long time.
It is ancient, deep groundwater made from pluvial (wetter) periods in the geological past
what are the 7 water stores in order from largest to smallest with their percentage and residence times?
1) oceans (96.9%, 3600)
2) cryosphere (1.9%, 15000)
3) groundwater (1.1%, up to 10000)
4) rivers and lakes (0.01%, 2 weeks-10 years)
5) vegetation (0.0001%, 1 week)
6) atmosphere (0.001%, 10 days)
7) soil moisture (0.001%, 2-50 weeks)
what are the 5 flows/transfers in order from largest to smallest with their size, measured in km cubed per year
1) ocean evaporation (400,000)
2) ocean precipitation (370,000)
3) land precipitation (90,000)
4) evapotranspiration (60,000)
5) surface flow (runoff) (30,000)
explain the problem of the availability of water
2/3 of water is locked in the cryosphere and so is inaccessible. water is fundamental for human life and for crops to grow. with population growth we need to ask ourselves how we are going to have enough water, it is a finite resource.
water vapour is the most important greenhouse gas and is driving climate change
distinguish the different flows of the hydrological cycle
interception- the retention of water by plants and soils which is subsequently evaporated or absorbed by the vegetation
infiltration- the process by which water soaks into, or is absorbed by the soil
percolation- similar to infiltration but a deeper transfer of water into permeable rocks
throughflow- the lateral transfer of water downslope through the soil
groundwater flow- the very slow transfer of percolated water through permeable or porous rocks
surface run off- the movement of water that is unconfined by a channel across the surface of the ground
channel or river flow- takes over as soon as the water enters a river or stream, the flow is confined within a channel
explain the future for our water
- climate change is altering out budget, cryosphere is melting and increasing the proportion stored in the oceans
- global population is rising, scheduled to reach 10 billion by 2055, water supply will not be able to keep up with pop growth
- accessible water is a mere 1% of all the world’s freshwater and so it is a scarce resource needing careful management
what are the 5 implications for future water security
- conflict over water sources (transboundary)
- drought and famine
- environmental refugees
- price of water increases
- more use of technology (e.g. desalination = further carbon emissions
is water renewable or non-renewable?
- water is generally considered a renewable resource but humans extract fossil water which is not recharged
- fossil water and crois-here are two water stores that are claimed to be non-renewable
explain the water budget
the global water budget limits water available for human use due to:
- only small % available for human use (96% salt water)
- 2/3 freshwater locked in cryosphere (long residence time), have to melt it
- most of the rest of the water is in the soil, vegetation or deep underground (some is fossil water)
the water stores have different residence times
what are fluxes?
he rates of flow between stores. the greatest fluxes occur over the oceans.
what is the global water budget?
it takes its account all the water that is held in stores and flows of the hydrological cycle, only 2.5% is freshwater. only 1% of fresh water is accessible.
what are the inputs in the drainage basin?
precipitation patterns and types:
- orographic
- frontal
- convectional
vary in a number of different ways. by form (rain, snow, hail), amount, intensity, seasonality, distribution
what are the flows in the drainage basin?
interception infiltration surface runoff saturated overland flow throughflow percolation groundwater flow river or channel flow
what are the outputs in the drainage basin?
evaporation- the process by which moisture is lost directly into the atmosphere from water surfaces, soil and rock
transpiration- the biological process by which water is lost from plants through minute pores and transferred into the atmosphere
discharge (channel flow)- into another, larger drainage basin, a rivulet, lake or the sea, the amount depends on the amount of precipitation falling directly into the channel
what type of system is a drainage basin?
it is an open system. it has inputs and outputs.
what is orographic precipitation?
also known as relief rainfall, relating to mountains, orographic uplift is when the uplift of an air mass, because of an orographic obstruction, causes the cooling of the air mass, If enough cooling takes place, condensation can occur and form into orographic precipitation, especially mountains and hills
what is frontal precipitation?
caused when warm air meets cold air and forces the warm air to rise to then 3C’s, creating low pressure, rises and then forms rain through clouds, as seen in the UK
what is convectional precipitation?
caused by when moisture evaporates and rises when heated by the sun (3C’s), in warm areas
what is saturated overland flow?
surface run off caused when soil is saturated (full of water)
what are the different parts of the drainage basin?
source
watershed- the edge of highland surrounding a drainage basin which marks the boundary between two drainage basins
tributary
confluence - the point at which two rivers or streams join
mouth