11 March 2016
Pep Canadell and Hanqin Tian
Pep Canadell is the Chief Investigator for the ESCC Hub’s Project 2.9: Risk assessment for future carbon sources and sinks.
Each year our terrestrial biosphere absorbs about a quarter of all the carbon dioxide emissions that humans produce. This a very good thing; it helps to moderate the warming produced by human activities such as burning fossil fuels and cutting down forests.
But in a paper published in Nature today, we show that emissions from other human activities, particularly food production, are overwhelming this cooling effect. This is a worrying trend, at a time when CO2 emissions from fossil fuels are slowing down, and is clearly not consistent with efforts to stabilise global warming well below 2ºC as agreed at the Paris climate conference.
To explain why, we need to look at two other greenhouse gases: methane and nitrous oxide.
The other greenhouse gases
Each year, people produce about 40 billion tones of CO2 emissions, largely from burning fossil fuels and deforestation. This has produced about 82% of the growth in warming due to greenhouses gases over the past decade.
The planet, through plant growth, removes about a quarter of this each year (another quarter goes into the oceans and the rest stays in the atmosphere and heats the planet). If it didn’t, the world would warm much faster. If we had to remove this CO2 ourselves, it would cost hundreds of billions of dollars each year, so we should be very grateful that the Earth does it for free.
Apart from CO2, there are two other main greenhouse gases that contribute to global warming, methane (CH4) and nitrous oxide (N2O). In fact, they are both more potent greenhouse gases than CO2. The global warming potential of methane and nitrous oxide is 28 and 265 times greater than that of CO2, respectively.
The human emissions of these gases are largely associated with food production. Methane is produced by ruminants (livestock), rice cultivation, landfills and manure, among others.
Other human-induced emissions of methane come from changes to land use and the effects of climate change on wetlands, which are major producers of global methane.
Nitrous oxide emissions are associated with excessive use of fertilisers and burning plant and animal waste. To understand how much excess nitrogen we are adding to our crops, consider that only 17 of 100 units of nitrogen applied to the crop system ends up in the food we eat.
Sinks and sources
Just as humans pump greenhouse gases into the atmosphere, the land also produces and absorbs them. If the land absorbs more of a gas than it produces, we think of it as a ‘sink’. If it produces more than it absorbs, we call it a ‘source’. The ability of the land to absorb and produce greenhouse gases is affected by human activity.
We wanted to know how human activities on the land are affecting these sinks and sources. Globally, the land currently absorbs more CO2 than it produces (we don’t include fossil fuels in this), so it is considered a carbon sink. But we found that this is overwhelmed by production of methane and nitrous oxide, so overall the land is a source of greenhouse gases.
This study highlights the importance of including all three major greenhouse gases in global and regional climate impact assessments, mitigation options and climate policy development.
Another recent study calculated that the size of this combined greenhouse gas source is about equivalent to the total fossil fuel emissions of CO2 in the 2000s. Looking at the chart below, if you add up the carbon emissions from the ‘LUC gross source’ (emissions from deforestation) and the emissions from methane and nitrous oxide (in blue and green), then you can see they are roughly equivalent to those from the combustion of fossil fuels.
So it’s a huge part of our contribution to climate change.
Importantly, CO2 emissions from deforestation together with methane and nitrous oxide emissions are mainly associated with the process of making land available for food production and the growing of food in croplands and rangelands.
Unfortunately, there has been limited discussion about major commitments to decarbonise the food production system, as there has been about decarbonising the energy system.
Countries, particularly emerging and developing economies, have shown little interest in placing the food system at the forefront of climate negotiations. One reason is what’s at stake: feeding their people.
A continuation of the current growth trends in methane and nitrous oxide emissions, at a time when growth of CO2 fossil fuel emissions is slowing, constitutes a worrying trend. The greenhouse gas footprint of food is growing while the role of the food system in climate mitigation is not receiving the attention that it urgently needs.
Opportunities for mitigation in this sector are plentiful, but they can only be realised with a concerted focus.
Pep Canadell is a CSIRO Senior Principal Research Scientist, and Executive Director of the Global Carbon Project, CSIRO and Hanqin Tian is Director, International Center for Climate and Global Change Research, Auburn University.