3.1.1 water and carbon cycles Flashcards
what is a system?
a system is a assemblage of interrelated parts that work together
contain a series of stores, components and have flows (connections) between them
what are a systems concepts?
inputs - matter or energy is added
outputs - matter or energy leaves
stores - matter or energy builds up
flows - matter or energy moves within the system
boundaries - limits to the system
what is a systems structure?
structure lies within a boundary, functioning with inputs and outputs
- elements = things that make up the system eg molecules
- attributes = characteristics of the elements that can be measured or percieved eg size, colour
- relationships = are the associations between the elements and attributes
what are cascading systems?
when the output of one system becomes the input to another
what are open systems?
a system in which both mass and energy are allowed to transfer across system boundary
flow of matter as well as energy in and out of the system
what are closed systems?
transfers of energy both into and out of the system boundary
no transfer of matter
what are isolated systems?
no interaction between system and surroundings
theoretical systems
describe both feedback loops and dynamic equilibrium
equilibrium = balance between inputs + outputs
negative feedback = effects of an action are nullified by its subsequent knock-on effects
positive feedback = effects are amplified or multiplied by subsequent knock on effects or secondary effects
what are the five types of systems in water and carbon?
- hydrosphere = water
- biosphere = living matter
- cryosphere = ice
- atmosphere = air
- lithosphere = rocks
what keeps living organisms alive?
recycling nutrients between organisms and environments
what is the water cycles closed system?
spends time in ocean, air, surfaces and ground water
solid, liquid and gases are interchangeable based on temperature
infiltration > groundwater > evapouration
precipitation > snow + ice > melting
what is the carbon cycles natural system?
chemically versatile elements
found in life forms, sedimentary rocks, diamonds, graphite, coal, oil and gas
stored in lithosphere, hydrosphere, cryosphere, atmosphere, biosphere
carbon sink is a store that absorbs more carbon than it releases
carbon source releases more carbon than it absorbs
what is the concept of dynamic equilibrium in the water cycle?
refers to the tendency towards a natural state of balance within the hydrological cycle
closed system cycle - no water enters or leaves. recycled around
drainage basin is a open system as inputs and outputs change
dynamic equilibrium is easily upset by storms and droughts
as well as human activity
what are the types of precipitation?
precipitation: water that falls to the surface of the earth from the atmosphere, including snow and hail
- convectional = warm air rises, condenses at higher altitudes and falls as rain
- relief = warm air is forced upward by a barrier eg mountains, causing it to condense at higher altitudes and falls as rain
- frontal = warm air rises over cool air. warm air is less dense and lighter so condenses at higher altitudes and falls as rain
what is evapotranspiration?
compromised of both evaporation and transpiration
evaporation = heated by the sun causing it to become a gas
transpiration = occurs in plants when they respire, releasing water which then evaporates by the sun
what is streamflow?
water that enters a drainage basin leaving through the atmosphere or streams that drain a basin
may flow as tributaries into rivers, oceans and lakes
what is infiltration?
process of water moving from above ground into the soil
grass crops and tree roots create passages for water to flow through, therefore increasing the infiltration capacity
precipitation falling at a greater rate than the infiltration capacity leads to overland flow
what is percolation?
water moving from the ground into porous rock or rock fractures
percolation rate is dependent on fractures and permeability of rock
what is throughflow?
movement of water through the soil into streams and rivers
speed of movement is dependent on the type of soil
clay soils have smaller pore spaces with a slower flow rate
sandy soils drain quickly because they have larger pore spaces and natural channels so have a quicker flow rate
what is surface run off?
water flowing above ground as sheet flow
what is ground water flow?
water movement through the rocks
what is streamflow?
water that moves through established channels
what is stemflow?
flow of water that has been intercepted by plants or trees down the plant
what are the five stores?
- soil water = stored in soil and utilisied by plants
- ground water = stored in pore spaces of rock
- river channel = stored in a river
- interception = water intercepted by plants before reaching the ground
- surface storage = water stored in puddles, ponds ect
what is the water cycle’s global distribution?
97% is global water
2.5% of stores is freshwater
69% is glaciers, ice caps and sheets
30% is groundwater
1% surface and other freshwater
oceans and water cycle
most of the water is stored as saline water
oceans cover 72% of the world but only 5% has been explored
salt allows oceans to remain liquid in temps below 0 degrees
pH has fallen from 8.25 to 8.14 in the past 250 years due to increased carbon
terrestrial water and water cycle
surface water
rivers make 0.0002% of water, covering 1,000,000 km2
lakes are collections of freshwater found in hollows
Canada has estimated 31,752 lakes
what is biological water?
constitutes the water stored in all the biomass, dependent on the vegetation
areas of dense rainforests, store more water
what are aquifers?
aquifers are underground water stores and on a global scale are unevenly distributed
30.1% of all freshwater is stored in rocks deep below the ground, forming vast reservoirs
commonly found in porous + permeable rocks such as chalk and sandstone
describe porous and clay soil and the effect on the storage of water
store of water varies in capacity to store or transfer water
porous sandy soil = holds very little water but allows transfer of water
clay soil = stores a huge amount of water but allows little transfer of water
what are the formats of cryospheric water?
- sea ice = does not raise sea levels, when it melts
forms from ocean water
ice shelves from ice sheets and glaciers move out over oceans
icebergs only raise sea levels when they leave the land - ice sheets = mass of glacial land exceeding 50,000km2
Antarctica and greenland account for 99%
form when winter snowfall doesn’t melt completely in summer
constantly moving downhill due to weight - ice caps = dome shaped and located over highest points of an upland area
- alpine glaciers = thick mass of ice found in deep valleys and upland hollows
- permafrost = ground that remains at or below 0 degrees for at least two consecutive years
thickness varies
melting permafrost releases huge CO2 + methane
what is the most common atmospheric state?
the most common state is water vapour
water vapour absorbs, reflects and disperses incoming solar radiation helping the atmosphere regulate it’s temperature
cold air cannot hold as much water vapour
an increase in water vapour will increase atmospheric temperature (positive feedback)
clouds are a visible mass of water droplets
what is the store residence time?
the amount of water in a store / rate of addition of water to store or loss
why does the water in soil not remain for long?
quickly percolates in bedrock
transpired by plants into the atmosphere
transferred in rivers by through flow
evaporated into atmosphere
what are the four movements of water?
- ablation = substance changes from a solid to liquid
- freezing = substance changes from liquid to solid
- vaporisation = substance changes from a liquid to vapour
- condensation = substance changes from a vapour to liquid
how does evaporation drive change in the magnitude of water? what are the rates dependant on?
rates dependant on:
amount of solar energy
availability of water
humidity in air
temperature of air
how does condensation drive change in the magnitude of water?
temperature is reduced to the dew point = temperature at which water vapour in the air turns into liquid water
when it air rises it cools, as it cools it expands
can occur when air is forced over hills = orographic effect
describe the process of water condensation
- the atmosphere is full of gas particles (water vapour) also particles such as salt and dust called aerosols
- water vapour and aerosols bump into each other. when the air is cooled some of the water vapour sticks to the aerosol
- the warmer the air the more water vapour it can hold. clouds form when the air rises, becomes saturated and cannot hold any more water.
- water droplets group together they become heavy and gravity pills them down as raindrops
how do clouds form?
from spatial and temporal changes in the water cycle
equator = high evapouration so air rises, cools, condenses to form low pressure zone (ITCZ)
mid latitudes = convergence of warm tropical air + cold artic air
localised scale = thunderstorms form from intense convective activity
how does frontal rainfall form?
- areas of warm and cool air are blown towards each other by the wind
- the lighter less dense warm air is forced to rise over the denser cold air
frontal rain produces a variety of clouds which bring moderate to heavy rain
how does relief (orographic) rainfall form?
- the most warm air is forced to rise. cools and condenses forming clouds
- the air drops down over the mountain warming as it does.
as it warms it increases the amount of water it can hold, meaning little rainfall occurs here. this is called the rainshadow effect. - the prevailing wind picks up moisture from the sea
how does convectional rainfall form?
- the surface of the earth is heated by the sun
- the warm surface heats the air above it. hot air always rises and as it does so the air begins to cool and condensate.
- convection produces cumulus-nimbus clouds which produce heavy rain and possibly thunder and lightening
what are cryospheric processes?
processes that has led to the climate being warmed leading to ice stores to shrink and retreat
positive feedback
how do hillslopes become a process of change?
considered to be most important local unit by hydrologists
area impacted by human and natural factors
consists of multiple water stores over short timescales
most influential process is infiltration and rapid transfer of water overland
short time scales
magnitude of store changes
influence of infiltration + overland flow
what influences do the seasons have on the soil water budget?
wet seasons:
precipitation exceeds evapotranspiration (water surplus)
ground store fills with water so higher discharge and surface run off
drier seasons:
evapotranspiration exceeds precipitation (ground store depletion)
some flows into the river channel but is not replaced by precipitation
back to wet seasons:
deficit of water
ground stores recharged
what is the soil water budget?
the changes in the soil water store during the course of a year due to infiltration
what is the field capacity in regards to the soil water budget?
soil holds as much water as possible with no outputs
dependant on type and depth of soil
texture and permeability
what is the bed rock in regards to the soil water budget?
capacity to store and transfer water dependant on lithology + structure
what is a drainage basin?
area of land drained by a river + tributaries, includes water found on surface soil + near surface geology
open system
casading system
what are the five features of a drainage basin?
source/mouth
tributary
river channel;
watershed
confluence
what is the water balance?
the balance between inputs and outputs
evapouration and transpiration
DIAGRAM ON NOTES
what is the equation for water balance?
precipitation (P) = Discharge (Q) + Evapotranspiration (E) +/- changes in storage
what is the rivers regime in regards to the water balance?
that the discharge levels rise and fall in a river, often showing an annual pattern
what is the equation for runoff variation?
discharge = cross sectioned x velocity