When one kilogramme of gas is evaluated against the
same amount of carbon dioxide in a stipulated time, we can find a measure of
the relative global warming contribution, technically known as Global Warming
Potential (GWP).The time span is significant to maintain uniformity in the GWP,
as each Greenhouse Gas (GHG) has a different life span in the atmosphere before
it breaks down or is removed. Normally, for official reports, a time span of
100 years is usually used. If a gas absorbs radiations of a wavelength
which is already being absorbed by the atmosphere, then the GWP is low, on the
other hand, if it absorbs light at a wavelength that normally passes through
the atmosphere (without being absorbed) then the GWP is high.
Gases
|
Formula
|
Lifespan
|
GWP
|
|||
20
|
100
|
500
|
||||
Carbon dioxide
|
CO2
|
Variable
|
1
|
1
|
1
|
|
Methane
|
CH4
|
12±3
|
72
|
25
|
7.6
|
|
Nitrous oxide
|
N2O
|
114
|
289
|
298
|
153
|
|
Sulphur hexafluoride
|
SF6
|
3200
|
16300
|
22800
|
32600
|
|
Chlorofluorocarbons
|
CFC12
|
45
|
1100
|
10,900
|
5200
|
|
Since the industrial revolution,
concentrations of greenhouse gases have increased linearly. The GHGs are found
to have a tendency to absorb and emit infrared (thermal) radiations. These
gas molecules have two or more component atoms, which are loosely bound, due to
which they vibrate on absorption of heat. When the
infrared radiations strike a molecule such as carbon dioxide and causes its
bonds to bend and vibrate (this is called the absorption of IR energy), the
molecule gains extra kinetic energy that may either be transmitted to other
molecules through molecular collision or be re-radiated back to the space,
earth causing a general heating of the earth and near surface atmosphere. The major components of the
atmosphere (N2 and O2) are two-atom molecules are tightly bound, and
so they cannot vibrate, as a consequence they neither absorb heat nor do they
contribute to the greenhouse effect. On the contrary it is believed that these
gases allow the radiations to pass through the (near surface) atmosphere.
Eg of effect of infrared radiations on CO2 gas.
The dips in the lines are caused by
the absorption of energy; hence only 10% of the energy is transmitted.
Due to accelerated anthropogenic activities
(combustion of fossil fuels, deforestation etc) and the long life span
(variable), the concentrations of CO2 are relatively high amongst all the other
gases making it the dominant GHG. Although water vapor is the real strongest
GHG in the atmosphere its concentration is kept in control due to precipitation
and so they are not as harmful as CO2.
I hope this blog helped in understanding why the GHG’s
cause global warming.
Thank you for reading, stay tuned there is a lot more
coming up.
Interesting. Details of GHG's and comparison with CO2 noteworthy.
ReplyDeleteNow I have a clearer understanding of the potential CO2 has to the atmosphere when comparing with other GHGs. Keep up your good work!
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