Natural gas as a ‘bridge’. Dangerous procrastination?
by Lindsay Wilson
There has been much talk of natural gas as a ‘bridge’ fuel lately, particularly due to its role in cutting
US carbon emissions.
From an economic or energy security point of view this might make some sense, but in terms of climate change natural gas is a half measure that risks dangerous procrastination.
If all the coal fired power stations in the world switched to natural gas tomorrow we wouldn’t go close to stabilizing atmospheric carbon dioxide concentrations.
Some simple carbon maths shows why we need to be more ambitious.
Carbon Emission SourcesFossil fuels have done wonders for economic development ever since the start of the industrial revolution. But if we want to keep on developing without toasting the planet we need to change how we get our energy.
For me, the easiest way to understand our carbon dioxide problem is to think of it in terms of ‘sources’ and ‘sinks’.
The main sources of man made carbon emissions are oil, coal, natural gas and land use change emissions. Whilst the main sinks for carbon emissions are the ocean, the land and the atmosphere.
In the last 50 years the amount of carbon dioxide mankind has emitted has grown dramatically, due to rising fossil fuel emissions.

Man made carbon emissions have grown by 150% since 1960.
The majority of this growth has come from oil, coal and natural gas with a smaller contribution from cement production and gas flaring. Land-use change emissions are down over the last decade because the net flux between deforestation and reforestation is slowly improving.
Carbon Emission SinksOnce carbon dioxide goes into the atmosphere it stays there for a long time. About 33% is still there after 100 years, and 20% is still in the atmosphere after 1000 years.
But when we think about where our emissions go it is simpler to look at the net change that occurs to the sinks each year. In this way global carbon emissions are balanced by the annual absorption of the ocean, land and atmospheric sinks.
The following chart shows where our human carbon emissions have gone over the last 50 years.

The oceans have absorbed 29% of man made carbon emissions since 1960. Land sinks including vegetation, soils and humus have absorbed 27%. Whilst 44% of carbon emissions have resulted in the growth of atmospheric carbon dioxide concentrations.
The light blue section of this chart is equivalent to the share of annual carbon emissions that ends up in the atmosphere. For each 7.8 Gt CO2 that remains in the atmosphere the atmospheric concentration of carbon dioxide rises by 1 ppm (parts per million). Between 2000 and 2009 we added an average of 15 Gt CO2 to the atmosphere each year resulting in atmospheric carbon dioxide concentrations rising by an average of 2 ppm each year. The growth rate last decade was higher than in any
earlier decade.
Between 1960 and 2010 growing carbon emissions have caused atmospheric concentrations of carbon dioxide to grow from 317 ppm to 389 ppm. If it wasn’t for the ocean and land sinks absorbing more carbon dioxide with both rising concentrations and rising emission rates we would already be pushing 500 ppm.
To stop the growth in the atmospheric carbon dioxide concentrations human carbon emissions would need to balanced by the sink capacity growth in the land and oceans. To slow the acidification of the oceans we would need to do much more.
The Scale of Our ProblemStabilizing atmospheric concentrations of carbon dioxide is the central challenge of climate change.
We also need action on other positive forcing agents like methane, nitrous oxide, ozone and black carbon, as well as further study of aerosol and cloud management, but without tackling carbon dioxide we cannot properly address climate change.
Although the most common way to highlight the scale of this challenge is as a
carbon budget between now and 2050, I find it much easier to understand by just thinking about one year. That way I’m not thinking about 2050, I’m thinking about what needs to happen today.
I’ll use 2010 as an example.

Based on global sources of carbon dioxide in 2010 and the average sink absorption over the last decade we would need to cut global emissions in half to stabilize atmospheric carbon dioxide concentrations. But in fact sinks absorption is also a function of emission rates, so this immediate cut in half would need to be quickly followed by more rapid emissions reductions to maintain stable concentrations. If technically possible we could also stabilize concentrations by doubling the rate at which carbon dioxide is absorbed by the oceans, land or possibly by some type of technology. But that technology is not really in existence.
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