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Before devling into a discussion about the possible important role of methane in global warming, let's first take a look at some early indicators that this process is now happening.
Note: On Thursday we will be using the laptops to do an exercise in "weather event" detection to see how difficult it is to find a real event buried in noisy climate data.
Table 1
Characteristics of some major (climate changing) greenhouse gases
Greenhouse gas |
Sources |
Sinks |
Importance for climate |
---|---|---|---|
Carbon Dioxide (CO2) |
1) Burning of fossil fuel 2) Land-use change (deforestation) |
1) Ocean Uptake 2) Plants!& photosynthesis |
Absorbs infrared radiation; affects stratospheric O3 |
Methane (CH4) |
1) Biomass burning 2) Enteric fermentation 3)Rice paddies |
1) Reactions with OH 2) Microorganisms uptake by soils |
Absorbs infrared radiation; affects tropospheric O3 and OH; affects stratospheric O3 and H2O; produces CO2 |
Nitrous Oxide (N2O) |
1) Biomass burning 2) Fossil-fuel combustion 3) Fertilizers |
1) Removal by soils 2) Stratospheric photolysis and reaction with O |
Absorbs infrared radiation; affects stratospheric O3 |
Ozone (O3) |
Photochemical reactions involving O2 |
Catalytic chemical reactions involving NOx, ClOx and HOx species. |
Absorbs ultraviolet and infrared radiation |
Carbon Monoxide (CO) |
1) Plant emissions 2) Man-made release (transport, industrial) |
1) Soil uptake 2) Reactions with OH |
Affects stratospheric O3 and OH cycles; produces CO2 |
Chlorofluorocarbons (CFCs) |
Industrial production |
Insignificant in troposphere, dissociated in stratosphere (photolysis and reaction with O) |
Absorbs infrared radiation; affects stratospheric O3 |
Sulphur Dioxide (SO2) |
1) Volcanoes 2) Coal and Biomass burning |
1) Dry and wet deposition 2) Reactions with OH |
Forms aerosols, which scatter solar radiation |
The Relative Importance of Methane:
Current concentration of CO2 is 366 ppm
Current concentration of CH4 is 1.8 ppm and is responsible for 20% of the greenhouse gases in the atmosphere (tho that 20% depends on how you model the ratio of IR absorption between CO2 and CH4.)
The relative absorption power of methane to carbon dioxide is still uncertain. The "offical" value of its GWP (global warming potential) is 21.
A more recent version of this table is below where the ranges in parantheses represent the uncertainy in the variable:
Distribution of wetlands emission and soil moisture potential:
Recent build up of methane in the atmosphere seems to closely follow
the world's population strong argument that build up
is human induced:
However, in recent years, there appears to be a leveling off of methane buildup. There is no viable explanation for this (yet) but we will speculate a bit.
Methane Removal Mechanism (some estimates suggest the methane residence time is up to 12 years so there is short term equilibrium control if methane emissions from earth's surface were reduced):
Atmospheric Chemistry End Result:
CH4 + 2O2 CO2 +
2H20
A recent finding shows that methane is more effectively processed by soil bacteria in an aspen/birch forest than in either a coniferous forest or grassland.
Under conditions of high soil mositure, the processing rate was up to 65% higher (this is quite significant).
If changing precipitation and temperature pattners serve to enhance the likely northward migration of these kinds of forces, then this is a biological negative feedback channel to global warming.
In the US, anthropogenic sources are stabilizing
This is also seen in the UK
But these results probably are insufficient
to explain the worldwide levelling off and there hasn't been sufficient
wetlands loss in the last 10 years to explain this either.
The most probable explanation, therefore, is the fall of the Soviet
Union:
A major concern, a positive feedback loop: (note: approximately 3000 times the current volume of methane in the atmosphere is currently stored in hydrate form).
Note, however, that "catastrophic" release of CH4 during period of Ice Ages may be the natural way that the Earth accelerates out of a glacial period. There is lots of evidence discovered in the last 2-3 years for such sudden warm ups in geologic history.
Known Hydrate deposits. Found typically in continental shelf where marine organisms (microbes) actively feed on carbon and carbon related productes to produce methane in the sediments.
Good overview of the hydrate "problem"
Methane is more directly related to food production and population
growth so it could also dominate in the near future
Frozen methane is also found in the Arctic Ice Caps and will
be released due to global warming thus exacerbating the problem. This
is far more serious that people realize. In the last 2 years, the scientific
community, however, has done lots of research on this problem and have
conclude its a potentially serious effect.