Peatlands, a growing net source of greenhouse gasses since 1960

December 1st, 2019 | Download as PDF
Peatlands, a growing net source of greenhouse gasses since 1960

Photo: Boreal and temperate peatlands have been drained for centuries and used for agriculture, forestry, and peat extraction, as on this photo in the Netherlands.

Ever since the last ice age, natural peatlands have been important carbon sinks, and intact peatlands still are today. However, drainage of peatlands for agriculture and forestry has transformed large areas from former sinks into net sources of greenhouse gasses. Especially in temperate and boreal regions, but increasingly also in the tropics. On a global scale, peatlands turned from a net sink into a net source of greenhouse gasses in 1960. Rehabilitation of these peatlands may greatly reduce additional emissions in the future.

Boreal and temperate regions versus the tropics

The distinction between boreal and temperate peatlands, and peatlands in tropical regions is important. Where the first group of peatlands experienced widespread land conversions by the nineteenth century, drainage onset in the tropics commenced only from 1960. Between 1850 and 2015, temperate and boreal regions lost 26.7 million ha, and tropical regions 24.7 million ha, of natural peatland. By 2100, the loss of natural peatlands in tropical regions may have increased to 36.3 million ha, corresponding to 62% of the initial peatland area in the tropics in 1850. The additional loss of peatlands in temperate and boreal regions will be small; total loss by 2100 is projected to be 7% of the initial peatland area in these regions in 1850.

Global balance 1850 - 2100

Drained peatlands not only emit CObut NHand N2O as well. These are all greenhouse gasses. The emission volumes of the latter two are also expressed in terms of COby translating their volumes into volumes of COthat have the same global warming impact. These volumes are expressed in volumes CO2e, where ‘e’ means carbon dioxide ‘equivalent’.

A reconstruction of the past and projections for the future were combined to estimate changes in the global balance of peatland greenhouse gasses for the period 1850 - 2100. For boreal and temperate peatlands annual uptake rate of greenhouse gasses by intact peatlands is projected to decrease from 0.31 (in 1850) to 0.29 Pg CO2e (in 2100), along with an increase in the drained area. For tropical peatlands a decrease from 0.10 to 0.04 Pg CO2e is projected. 1Pg = 1012kg.

In the context of the global budget of greenhouse gasses this change in uptake (sink) is relatively small. The change in emissions (source) is much more pronounced, however. Estimates for the period 1850 - 2100 show a steady increase of emissions from peat decomposition. For 2015, a release of greenhouse gasses from drained peatlands of 1.53 ± 0.80 Pg CO2e is estimated, with 1.26 ± 0.77 of that total emitted in the tropics.

Dominant contribution tropics since 1980

Emissions from temperate and boreal systems dominated the overall picture until around 1980. Since then, annual emissions from the tropics exceed those from temperate and boreal regions. By 2100, tropical regions are projected to completely dominate greenhouse emission from peatlands. Without counteracting measures having been taken, the annual emissions rate will then reach 2.23 ± 0.69 Pg CO2e in the tropics, compared with ‘only’ 0.07± 0.16 Pg CO2e in boreal and temperate regions. In the latter regions, most of the carbon will have disappeared by oxidation by then. In drained tropical peatlands this exhaustion will start after 2100 because of the later drainage onset.

Between 1850 and 2100, drained peatlands will have released 249 ± 38 Pg CO2e by biological peat oxidation. From 2015 onwards, the release will total 169 ± 44 Pg CO2e, dominated by tropical emissions.

No more net emissions from peatlands?

These results illustrate the strong dominance of sources over sinks. What would it take for global peatland sources to equal peatland sinks, and thus for peatlands to become neutral in terms of emissions of greenhouse gasses by 2050 and thereafter? Almost all drained peatlands need to be rehabilitated. Full rehabilitation of all degraded peatlands in boreal and temperate regions, and of 98% of degraded peatlands in the tropics is needed for this.

Stop global warming at +2 °C?

The IPCC has estimated in 2014 that a net emission of about 2,550 - 3,150 Pg CO2e since 1870 would allow global mean air temperatures to remain below +2 °C. Without counteracting measures, the emissions from drained peatlands will consume 7.9 to 9.8 % of this amount. Most of this ‘allowed’ budget has already been used, however, due to the already high anthropogenic emissions accumulated since 1870. The available budget left for 2020 - 2100 is only about 400 - 1,600 Pg CO2.

Rehabilitation of peatlands

Without rehabilitation of peatlands and with continued land conversion in the tropics, the emissions from peatlands may comprise 12-41% of the total remaining budget (from now on) of greenhouse gasses that would keep global warming below +2 °C. Widespread rehabilitation of formerly drained peatlands would substantially reduce these values to 3-12% of the budget. If we include extant peatlands in the overall calculation, the contribution of peatlands to this total ‘allowed’ budget would reduce to ‘only’ 1-5%.


Source: Leifeld et al., 2019. Nature Climate Change 9(12): 945-947.