Water and carbon cycle Flashcards
input
material or energy moving into the system from outside
output
material or energy moving from the system to the outside
energy
power or driving force
positive feedback
a cyclical sequence of events that amplifies or increases change
negative feedback
a cyclical sequence of events that nullifies or decreases change
open system
energy and matter are transferred over the system boundary
closed system
energy, not matter, is transferred over the system boundary
isolated system
nothing leaves
oceans cover…% of the earth’s surface
72%
pH of the oceans
alkaline of 8ish
features of cryospheric water
sea ice, ice sheets, ice caps, alpine glaciers, permafrost
sea ice
doesn’t raise sea levels when melted as already counts as sea
ice sheets
a mass of glacial land ice extending more than 50 000 km^2
ice caps
thick layers of ice on land that are smaller than 50 000 km^2
alpine glaciers
thick masses of ice found in deep valleys or in upland hollows
oceans contain …% of the earth’s water
97%
permafrost
when the ground remains frozen for two consecutive years
features of terrestrial water
rivers, surface water, lakes, wetlands, groundwater, biological water
lakes
greater than 2 hectares in area (anything less is a pond)
wetlands
areas of marsh, fen, peatland, or water
groundwater
water that collects underground in the pore spaces of rock at a depth of 4000m
major stores of water
oceanic water, cryospheric water, terrestrial water, atmospheric water
sublimation
when a solid becomes a gas without becoming a liquid
deposition
when a gas becomes a solid without becoming a liquid
latent heat in condensation
released during condensation as the gas molecules slow down and join together so the surroundings are warmed
latent heat in evaportation
absorbed during evaporation to give energy to break the molecular bonds, this means that the surroundings are warmed
…% of water is readily availible for human use
2.5%
factors affecting the rate of evaporation
solar energy, amount of water, humidity, temperature of the air
transpiration
where water is transported from the roots of a plant, to its leaves, and then lost through the poreson the leaf surface
evapotranspiration
the total output of water from the drainage basin directly into the atmosphere
factors affecting the rate of condension
temperature of the air, temperature of the surface
dew point temperature
colder air holds less water, the temperature when it’s cooled to saturation is the dew point temperature
condensation nuclei
the tiny particles, such as smoke, salt, and dust, that water vapour condenses on
why must the condensation nuclei be below the dew point temperature but above freezing point
so that the water vapour doesn’t sublimate
inputs in the water cycle
precipitation
outputs in the water cycle
transpiration and evapotranspiration (can also include run off)
flows/transfers in the water cycle
infiltration, stem flow, overland flow, through flow, groundwater flow, percolation, channel flow
through flow
when water flows through the ground
groundwater flow
slow movement of goundwater
percolation
water moves down through the ground
stores/components in the water cycle
groundwater, soil water, surface storage, channel storage
water balance
the difference between the inputs and outputs (and the subsequent change in storage) in the drainage basin
equation for water balance
P = Q + E +/- S P is precipitation Q is total run off E is evapotranspiration S is storage in soil and rock
soil moisture budget
the change in the amount of water stored in the soil throughout the year
factors affecting the soil moisture budget
climate, variation of temperature during the year, precipitation, time between precipitation
factors causing a variation in run off rates
saturated soil, rock type, type of precipitation, vegetation, evapotranspiration rate, intensity of precipitation
river discharge
the volume of water in a river in a m^3 at a given time
how do you calculate the discharge?
cross sectional area x speed = cumecs (m^3/s)
river regime
the variability in the river’s discharge throughout the course of the year in response to precipitation, temperature, evapotranspiration, and drainage basin characteristics
factors affecting river flow patterns throughout the year
climatic variation, land use changes, water abstraction, landscapes, geological characteristics
physical factors affecting the water cycle over time
extreme weather events, drought, precipitation levels, vegetation, evaporation rates, soil properties, relief, desertification
human factors affecting the water cycle over time
deforestation and afforestation, urbanisation, farming, water abstraction, irrigation methods, desertificaion
how does deforestation impact the water cycle?
decreases atmospheric feedback and so decreasing rainfall and increasing discharge
agricultural soil drainage
this is where excess water is removed from the soil, it’s a costly process but has many advantages
advantages of agricultural soil drainage
improved soil structure, improved areastion in the soil
how does agricultural soil drainage affect the water cycle?
speeds the through flow in soil artificially which means that more water reaches the rivers quickly so increased risk of flooding
water abstraction
when water is pumped out of the ground for use eg London
El Nīno
When the temperature rises around the tropical ocean it occurs every 5 years ish
Affects of el nīno in northern Australia and Indonesia
They experience dry weather
Affect of El Niño in South America
Lots of rain
How does drought affect the water cycle
Soil is baked so more surface flow, vegetation cannot survive, shortages in all water supplies (atmospheric, surface, ground)
What are the main stores of carbon
Lithosphere, hydrosphere, cryosphere, atmosphere, and biosphere
Carbon sink
A store that absorbs more carbon than it release
Carbon source
A store that releases more carbon than it absorbs
Carbon transfer
These are processes that transfer carbon between the stores
GtC
A gigatonne of CO2 is used to measure the amount of carbon in stores (1GtC=10^9 tonnes)
Anthropogenic CO2
CO2 generates by human activity
Greenhouse gas
Any gaseous compound in the atmosphere that is capable of absorbing infrared radiation thereby trapping and holding heat
Lithosphere
The crust and upper mantle this constitutes the hard and rigid outer layer of the earth
Weathering
The breakdown of rocks in situ by a combination of weather, plants, and animals
Biosphere
The total sum of all living matter
Carbon sequestration
The capture of CO2 and putting it into long term storage