water and carbon Flashcards
What is the water cycle
is a continuous cycle of water between the land and the atmosphere
It is a closed system
what are inputs of water
precipitation
what are the stores of water
atmosphere- clouds
groundwater
vegetation
what are flows of water
surface run off
through flow
groundwater flow
what are outputs of water
evaporation
what are stores of water
lithosphere - land
hydrosphere- water
cryosphere - frozen water (snow and ice)
atmosphere - air
biosphere - plants
what is the hydrosphere
water
largest water store
97% of all of earths water is stored in the ocean, with only 3% being stored as freshwater
out of the 3 % of freshwater, 30% is stored as groundwater,
0.3% is stored as liquid freshwater on the earths surface
what is the cryosphere
frozen water- snow and ice
examples:
-sea ice: ice that floats on the surface of the water, and varies with the seasons. It reflects solar energy so has a high albedo
-ice shelves: platforms of ice extending over the oceans
when they break off, it causes sea levels to rise
-ice sheets: glacial land that extends 50,000km over the ocean
-Greenland - if it was to melt, sea levels rise by 6m
-Antarctica-if it melts, sea levels rise by 60m
-ice caps: smaller ice sheets (less than 50,000 km)
mainly found in mountainous areas
-permafrost: soil/rock/sediment which has frozen for over 2 years
when it melts, releases methane
what is the global distribution of water stores?
-Unevenly distributed
-those countries with a higher latitude and altitude have more stored in the cryosphere
-some countries have more rivers
-some countries have more permeable geology, so more water stored underground in aquifers
-depends on climate- can affect evaporation rates
What is a positive feedback loop
where the changes in a system increase, and is permanently changed from the original system
what is negative feedback loop
changes happen, but the system eventually stabilises, and goes back to dynamic equilibrium
what is dynamic equilibrium
where the inputs and outputs of water are balanced
can be changed by:
-over abstraction of water
-flooding
-drought
what is a drainage basin
an area that gets drained by a river and its tributaries
-it is an open system
-inputs: precipitation
-outputs: evapotranspiration, run off
-stores: interception, soil/surface, groundwater
-flows: infiltration, throughflow, stemflow, overland flow
3 different types of rainfall
Frontall
Convectional
Relief/Orographic
What is frontall rainfall
where warm air is forced to rise and form clouds
what is convectional rainfall
long periods of warm weather which forms cumulonimbus clouds
what is relief/orographic rainfall
warm air is forced to rise over mountains which cools and condenses to form clouds
factors affecting change in magnitude of water stores over time and space
1- evaporation
2- cloud formation and precipitation
3-condensation
4- processes at hill slope
5-cryospheric processes
evaporation
when liquid changes to a gas
-can happen from surface of any water store
-rate varies globally and with seasons
-areas in tropical/subtropical have higher rates due to having more net radiation and being warmer
factors affecting rate:
-availability of water
-humidity of water- closer to saturation point, lower evaporation rate
-temperature of air- warmer air holds more water vapour
causes of precipitation and cloud formation
- warm air rises, forms a band of low air pressure- known as ITCZ- driven by heat, so follows the sun.
The ITCZ is formed between 2 hadley cells, where there is intense convectional rainfall
-Global atmospheric circulation system identifies areas of rising and falling air.
Converges warm moist air from the tropics with cold air from the Arctic to create frontall rainfall
Condensation
water vapour can condense to form liquid or solid, when air containing WV cools to its dew point- point at which it changes from a gas to a liquid.
- needs something to condense on- known as condensation nuclei
processes at hill slope
-Deforestation - less water intercepted, less in biosphere and lithosphere, more in hydrosphere
-Seasonal changes- in winter, more in cryosphere
-increased permeable surfaces
-storms- increased rainfall - less in atmosphere
Cryospheric processes
There has been 5 major global glacial periods in earths history- most recent starting 2.58 million years ago to present- the quaternary period.
-Glacial period- more water is stored as ice, sea levels are 120 m lower. process of accumulation
-Interglacial period- temperatures rise- ice melts- ablation
less water stored in the cryosphere
The water balance
-Balance between inputs and outputs
affects how much water is shored in the basin
worked out by:
precipitation=runoff + evapotranspiration
-within the Uk it varies with seasons:
-in winter, more precipitation than evapotranspiration- water surplus
-in summer- more evapotranspiration than precipitation - water defecit
Runn off
water that arrives to the river as surface run off or throughflow
Factors influencing:
-precipitation
-climate eg. drier climate- precipitation onto baked ground leads to run off
-rock type- if its impermeable, wont be able to infiltrate and get to river as overland flow
-human activity- deforestation- less interception
Human changes in the water cycle
1- farming
-growing demand due to consumerism
-more deforestation, less interception, more overland flow
-overgrazing cattle- compact the ground and make it impermeable, no infiltration and increased overland flow.
2- land use changes
-increase in population and consumerism- leads to rapid urbanisation, increases deforestation, increases impermeable surfaces
3-water abstraction
water is abstracted from stores when there is a high demand
-as population grows, growing demand for food and irrigation, water is abstracted from lakes, rivers, undergrounds- lead to the depletion of stores
Natural changes in the water cycle
1- storm events- this is due to high evaporation rates eg. temperature being 27 degrees for several weeks
-leads to intense low air pressure systems, falls as convectional rainfall
-natural process but disrupts the dynamic equilibrium and water stores
-uk-winter, us- summer
2: seasonal changes
-in summer, higher evaporation, more in the atmosphere and less in lithosphere
-itcz creates distinct wet and dry seasons
-in winter, less vegetation so less interception
-Uk faces atlantic depressions due to a change in air mass
3-Climate change
-influences storm events and seasons
climate has always changed, in a quaternary period
-periods of glacial and interglacial
-humans can induce climate change, through burning of fossil fuels
-cryosphere store melting at a quicker rate, sea levels rise rapidly- a positive feedback loop
The Eden Basin
The river Eden is located in north west of England between lake district and pennies
-some areas are 700 m above sea level
Uks prevailing wind comes in from the south west.
Warm air is forced to rise over mountains, and form orographic rainfall
-Eden receives average 2800mm of rain, where rest of uk is 920
-steep slopes with impermeable surfaces
-Highest ground is impermeable with thin soils- saturate faster
-only 1% is urban
-upper catchment is made of mountains-
-Hellvelyn-3rd highest in england-950m above sea
-Skiddaw-6th-930m
-impermeable surfaces
-24,000 people live there