Human activities Carbon cycles impacts
systems Cloud formation + precipitation
is added precipitation two air masses Farming Practices -
ploughing increases Atmosphere climate-affects greenhouse
and
Inputs matter or energy Frontal -
impacts the temperatures
infiltration , Crops increase infiltration and
-
gases , which
or energy leaves Of different temp meet , warm is forced
outputs matter
evapotranspiration . Livestock trample ground Land-carbon Cycle impacts plant growth
-
stores-matter or energy builds up up then cools forming precipitation
and reduce . Irrigation Can increase
infiltration and vegetations carbon stores
flows matter or energy moves orographic precipitation -
Warm air is
runoff and depleat groundwater stores
more CO2 in Oceans increases the
-
forced to rise over mountains, cools-rain deforestation reduces Oceans
boundaries limits of the system
-
-
Land use change -
convective Precipitation Sun heats the interception
-
Ocean acidity killing marine organisations
-
open system means both energy
matter can enter and leave
and
ground , moisture evaporates and rises in decreases the removingleft
permable a with calcium carbonate shells Also affects
.
a column of
warm air , as it rises it cools
layers prevents infiltration + increases run-off
organisms that are temp Sensetive Warmer
.
.
closed matter can't enter or water can't absorb as much CO2
system
-
take water from stores
-
processes water abstraction
cryospheric
-
leave but can enter / leave
energy to meet populations demand , extract more water and Carbon
during periods
of global cold , in puts to
-
Feedback water in dry seasons for irrigation both water and carbon are vitor for life as
the cryosphere are greater than outputs
-
Carbon is contained in all things and water is
small variations in the inputs and
during periods of warmer global temps, carbon Cycle needed for survival
-
-
lots of
water acid rain
on carbon combines with
out puts , tend to remain balanced magnitude of the store reduces as losses can be found in all of Earth's subsystems
, -
water is needed for photosynthesis which
-
from melting are greater than in puts
equilibrium
-
average = dynamic with 99 9 % in the lithosphere in rocks andthen removes carbon from the atmosphere
.
Positive feedback-amplify changes Drainage Basins . 04 % stored in the
0 deep ocean or surface - amount of CO2 affects temperatures and
the amount of evaporation and precipitation
temprises > ice cover melts >
- less ice area around the river where rain falling Carbon cycle is a closed system
-
-
-
Feedback cycles
cover means more sun energys reflected there flows into the river-boundary called
>
-
more energy is being absorbed by the the watershed. They are open systems water-positive temp rises - > increased
earth -> more temprise
evaporation - ↑ atmospheric water vapour
Negative feedback-counteracts change increases - greenhouse effect - rise in temp
lots of CO2 emitted -
> atmosphere CO2 rises water-negative temprise increased to form
> more water vapour
>
- > the
extra CO2 increases plant growth -
evaporation -
> temp fall
clouds -
> reflect suns
energy back -
plants remove and store more CO2 -
> the
carbon-positive temprises - > increased
amount of CO2 in atmosphere decreases plant respiration -> increased
atmospheric
> temprises
subsystems
-
CO2- greenhouse effect
Carbon-negative Atmospheric CO2
Cryosphere-all parts of the Earth where
increases -> increased plant
-
growth
its cold enough for water to freeze remove + Store (82-reduces CO2
plant
Lithosphere-crust and upper parts of Climate change
the Mantle (outermost Part of Earth)
water balance -
change patterns of precipitation-water
Biosphere-part where living things are Temporal + Spatial scale Shortages and conflict
-
affects how much water is
is
g plants , animals , bacteria
-morefrequent extremeweathere
found e stored in the basin
Temporal-carbon flows quickly during
.
rain-water
Hydrosphere-all of the water on Earth , wet season
photosynthesis , respiration , combusion and
-
rise in sea levels
surplus-river levels rise
-
liquid solid or gas form
in ,
.
deposition but takes time for sequestration effect of rise in temp on marine animals
dry season use up stores ,
-
-
=
Atmosphere-layer of gas between the
Spatial-photosynthesis is main flow for
Humans influence
and less precipitation
Earth's surface and space .
plants but combustion is more important at
-
all interlinked-matter and energy moves Hydrographs an ecosystem scale
-
Intergovernal Panel on ClimateChange
to lower human
river discharge-volume of water flowing States countries need
between the subsystems forms a -
Natural processes emitted CO2 to prevent large temprise
-
per second (cubic meters per second) more
cascading system Individual-use public transport ,
discharge Show the Wildfires -rapidly release carbon stored in
-
Hydrographs over
, energy efficient
fuel efficient cars
homes
biomass, less vegetation to remove carb on
water cycle hydrographs focus on the time , flood reliance on
river discharge at the time of a storm from atmosphere . Can encourage new plant Regional/National-reduce
renewable energy
hydrosphere contains 1 4 sextillion litres fossil fuels , reduce
.
-
water-less than 3 % is fresh water Influenced by : growth from ashes
negatives costs improve public
-
balance out
, transport more
Of
volcanic activity-releases carbon stored in afforestation schemes , green spaces ,
,
is size
O t drainage
of the freshwater only 3 % liquid
-
0 .
than capture + storage
-
freshwater in lakes or rivers and not
Dasin-small-less lag Earths Crust as
magina , less CO2 humans invest in Carbon
Global-international treaties
to
-
everyone has the ability to access it
.
-
shape of drainage Human impact carbon
basin-circle-flashy reduce greenhouse gasses ,
Evaporation -
Steepness-steep-Fossil fuels-extracting and burning trading schemes to hold accountable
releases CO2 that would be sequestered
magnitude of evaporation varies with time
less lagtype-flashy if
-
. Highest rates of
location and season CK Deforestation reduces carbon store , it
-
soil purned it releases co2
evaporation when theres lots of solar imperable rock + to atmosphere
radiation , lots of water , warm any air
Physical factors Farming practices- ploughing releases (O2 ,
rice paddies release Methane animals
condensation storms and precipitation precipitation ,
-
can't release both CO2 and Methane
increases peak discharge , some stores
.
on the amount of
magnitude depends Land use change-removing
had enough = mnoff , increases flows
comvegetationaction
-
water vapour in the atmosphere and the
Seasonou changes and vegetation-size of reduces
the Carbon store ,
temperature (dew point when water cools
Stores varies with seasons . Vegetation releases lots of CO2
Slower
intercepts precipitation
=
.
to the river channel
movement of water
doesn't reach
more vegetation more water
= .
systems Cloud formation + precipitation
is added precipitation two air masses Farming Practices -
ploughing increases Atmosphere climate-affects greenhouse
and
Inputs matter or energy Frontal -
impacts the temperatures
infiltration , Crops increase infiltration and
-
gases , which
or energy leaves Of different temp meet , warm is forced
outputs matter
evapotranspiration . Livestock trample ground Land-carbon Cycle impacts plant growth
-
stores-matter or energy builds up up then cools forming precipitation
and reduce . Irrigation Can increase
infiltration and vegetations carbon stores
flows matter or energy moves orographic precipitation -
Warm air is
runoff and depleat groundwater stores
more CO2 in Oceans increases the
-
forced to rise over mountains, cools-rain deforestation reduces Oceans
boundaries limits of the system
-
-
Land use change -
convective Precipitation Sun heats the interception
-
Ocean acidity killing marine organisations
-
open system means both energy
matter can enter and leave
and
ground , moisture evaporates and rises in decreases the removingleft
permable a with calcium carbonate shells Also affects
.
a column of
warm air , as it rises it cools
layers prevents infiltration + increases run-off
organisms that are temp Sensetive Warmer
.
.
closed matter can't enter or water can't absorb as much CO2
system
-
take water from stores
-
processes water abstraction
cryospheric
-
leave but can enter / leave
energy to meet populations demand , extract more water and Carbon
during periods
of global cold , in puts to
-
Feedback water in dry seasons for irrigation both water and carbon are vitor for life as
the cryosphere are greater than outputs
-
Carbon is contained in all things and water is
small variations in the inputs and
during periods of warmer global temps, carbon Cycle needed for survival
-
-
lots of
water acid rain
on carbon combines with
out puts , tend to remain balanced magnitude of the store reduces as losses can be found in all of Earth's subsystems
, -
water is needed for photosynthesis which
-
from melting are greater than in puts
equilibrium
-
average = dynamic with 99 9 % in the lithosphere in rocks andthen removes carbon from the atmosphere
.
Positive feedback-amplify changes Drainage Basins . 04 % stored in the
0 deep ocean or surface - amount of CO2 affects temperatures and
the amount of evaporation and precipitation
temprises > ice cover melts >
- less ice area around the river where rain falling Carbon cycle is a closed system
-
-
-
Feedback cycles
cover means more sun energys reflected there flows into the river-boundary called
>
-
more energy is being absorbed by the the watershed. They are open systems water-positive temp rises - > increased
earth -> more temprise
evaporation - ↑ atmospheric water vapour
Negative feedback-counteracts change increases - greenhouse effect - rise in temp
lots of CO2 emitted -
> atmosphere CO2 rises water-negative temprise increased to form
> more water vapour
>
- > the
extra CO2 increases plant growth -
evaporation -
> temp fall
clouds -
> reflect suns
energy back -
plants remove and store more CO2 -
> the
carbon-positive temprises - > increased
amount of CO2 in atmosphere decreases plant respiration -> increased
atmospheric
> temprises
subsystems
-
CO2- greenhouse effect
Carbon-negative Atmospheric CO2
Cryosphere-all parts of the Earth where
increases -> increased plant
-
growth
its cold enough for water to freeze remove + Store (82-reduces CO2
plant
Lithosphere-crust and upper parts of Climate change
the Mantle (outermost Part of Earth)
water balance -
change patterns of precipitation-water
Biosphere-part where living things are Temporal + Spatial scale Shortages and conflict
-
affects how much water is
is
g plants , animals , bacteria
-morefrequent extremeweathere
found e stored in the basin
Temporal-carbon flows quickly during
.
rain-water
Hydrosphere-all of the water on Earth , wet season
photosynthesis , respiration , combusion and
-
rise in sea levels
surplus-river levels rise
-
liquid solid or gas form
in ,
.
deposition but takes time for sequestration effect of rise in temp on marine animals
dry season use up stores ,
-
-
=
Atmosphere-layer of gas between the
Spatial-photosynthesis is main flow for
Humans influence
and less precipitation
Earth's surface and space .
plants but combustion is more important at
-
all interlinked-matter and energy moves Hydrographs an ecosystem scale
-
Intergovernal Panel on ClimateChange
to lower human
river discharge-volume of water flowing States countries need
between the subsystems forms a -
Natural processes emitted CO2 to prevent large temprise
-
per second (cubic meters per second) more
cascading system Individual-use public transport ,
discharge Show the Wildfires -rapidly release carbon stored in
-
Hydrographs over
, energy efficient
fuel efficient cars
homes
biomass, less vegetation to remove carb on
water cycle hydrographs focus on the time , flood reliance on
river discharge at the time of a storm from atmosphere . Can encourage new plant Regional/National-reduce
renewable energy
hydrosphere contains 1 4 sextillion litres fossil fuels , reduce
.
-
water-less than 3 % is fresh water Influenced by : growth from ashes
negatives costs improve public
-
balance out
, transport more
Of
volcanic activity-releases carbon stored in afforestation schemes , green spaces ,
,
is size
O t drainage
of the freshwater only 3 % liquid
-
0 .
than capture + storage
-
freshwater in lakes or rivers and not
Dasin-small-less lag Earths Crust as
magina , less CO2 humans invest in Carbon
Global-international treaties
to
-
everyone has the ability to access it
.
-
shape of drainage Human impact carbon
basin-circle-flashy reduce greenhouse gasses ,
Evaporation -
Steepness-steep-Fossil fuels-extracting and burning trading schemes to hold accountable
releases CO2 that would be sequestered
magnitude of evaporation varies with time
less lagtype-flashy if
-
. Highest rates of
location and season CK Deforestation reduces carbon store , it
-
soil purned it releases co2
evaporation when theres lots of solar imperable rock + to atmosphere
radiation , lots of water , warm any air
Physical factors Farming practices- ploughing releases (O2 ,
rice paddies release Methane animals
condensation storms and precipitation precipitation ,
-
can't release both CO2 and Methane
increases peak discharge , some stores
.
on the amount of
magnitude depends Land use change-removing
had enough = mnoff , increases flows
comvegetationaction
-
water vapour in the atmosphere and the
Seasonou changes and vegetation-size of reduces
the Carbon store ,
temperature (dew point when water cools
Stores varies with seasons . Vegetation releases lots of CO2
Slower
intercepts precipitation
=
.
to the river channel
movement of water
doesn't reach
more vegetation more water
= .
