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Geography
Carbon Cycle
Atmosphere
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Created by
Elsie Coote
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Cards (11)
fluxes
into the atmosphere
lithosphere
->
eruption
of gases
hydrosphere
->
diffusion
(evap)
biosphere->
respiration
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Fluxes
out of Atmosphere
hydrosphere->
diffusion
biosphere->
photosynthesis
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stores
in the atmosphere
mostly
CO2
some as
methane
(CH4)
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duration of carbon in the atmosphere
varies-
seconds to few hundred
years
though very much
shorter
than lithosphere
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fluctuation
of carbon in the atmosphere
rises at
night
with
respiration
drops during day with increased
photosynthesis
and great fluctuations during
summer
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Keeling
Curve
graph to show the measurement of
atmospheric
carbon
measured
daily
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natural
greenhouse effect
without greenhouse gases the average temperature, -6 compared to average
15
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CO2
vs
CH4
CO2
:
lasts longer
(
300-1000
vs 12-120)
is
more
(
8xmore co2
)
CH4
:
in
two years traps 80x more heat
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Carbon-14
dating
Process of estimating age of once living material by measuring the amount of
radioactive isotope
of
carbon
present in material.
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Short
wave vs long wave radiation
short-
more energy, arrives first (
blue
)
long-
less energy, reflected by earth (
red
)
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what % of short wave light gets to the earths surface?
50%-
then reflected and can
no longer
leave the atmosphere
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