- Carbon emissions due to tropical deforestation are accelerating, a new study has found.
- Using detailed maps of forest change as well as aboveground and soil carbon deposits, the researchers demonstrate that annual emission more than doubled between 2015-2019, compared with 2001-2005.
- Though the study reveals that the world has not met its commitments to stem deforestation, the authors say it also reveals that investments in forest protection and restoration are critical to addressing climate change.
The rate at which carbon escaped from the deforestation of tropical forests more than doubled in the first two decades of the 21st century, according to new research.
Earlier assessments relied primarily on government statistics on the land, which “painted a much different picture,” Paul Elsen, a climate adaptation scientist with the Wildlife Conservation Society and a co-author of the paper, said in an interview. That picture was one in which tropical deforestation is still a serious problem, with each razed hectare of quality forest representing the loss of wildlife habitat, ecosystem services and the ability to continue siphoning carbon from the air. But the calculations of the amount of carbon lost from deforestation around the world suggested the emissions from this major source of atmospheric carbon had stabilized or even started dropping.
At the same time, members of the team had previously documented the worrisome expansion of deforestation into mountainous forests in Southeast Asia. Their analyses showed these higher-elevation forests had a “massive carbon stock,” said lead author Yu Feng, a doctoral student at the Southern University of Science and Technology (SUSTech) in China. They found that the annual figures for the amount of carbon emitted when cleared were “unprecedented,” which they reported in a 2021 study published in the journal Nature Sustainability.
Surprised to find such a little-known source of substantial carbon emissions, the team decided to take a global look at the problem and determine whether these high rates were confined just to Southeast Asia.
To do that, though, they needed a more detailed understanding than that provided by the “bookkeeping” studies used by countries to ballpark forest carbon loss, Elsen said.
“[These studies] don’t locate in space [via satellites] where the forest loss is occurring and how much carbon is there,” he said. Improvements in satellite technology and the monitoring work that remote-sensing scientists such as Matt Hansen and his colleagues are doing at the University of Maryland have put more detailed information at the fingertips of researchers around the world, Elsen added.
“We’re in sort of a golden era of data sets that enables us to look at this very, very precisely,” he said.
The maps and data that Hansen and his team make available can tease apart what has happened to forests since the turn of the century. The data set has a resolution of 30 square meters (323 square feet), making it much “more reliable” than tabulations based on government-gathered statistics, Feng told Mongabay.
Elsen, Feng and their colleagues then used several other maps that plot out forest and soil biomass to estimate the amount of carbon held by the deforested areas mapped by Hansen’s team. The carbon found below the ground — in root systems and the soil, for example — typically takes longer to bleed into the atmosphere after deforestation than the carbon in aboveground sources, such as the trees’ trunks. But the team concluded this discrepancy wouldn’t change the overall trend in the amount of carbon lost, so they bundled the above- and below-ground carbon into a single statistic known as “committed loss.”
The researchers found that the world’s tropical forests emitted nearly 2 billion metric tons of carbon per year between 2015 and 2019, the final five years of the study period. That’s roughly equivalent to the annual emissions of 1,900 coal-fired power plants and more than twice the yearly tabulated forest carbon loss between 2001 and 2005.
The team reported their findings online Feb. 28 in the journal Nature Sustainability.
“It’s definitely concerning that their findings are that there’s a doubling of carbon loss just in two decades,” said Giuseppe Molinario, a geographer with the World Bank who was not involved in the research. Molinario said the study will likely confirm what many researchers suspected — that there’s been “an underestimation of the carbon loss.”
“It would follow that it’s somehow in sync with how much forest cover loss we’re seeing,” he added.
As the team drilled into the data, they uncovered regional patterns in where — and when — forest carbon loss occurred. For example, a lot of the carbon emissions in the early 2000s came from parts of the Brazilian Amazon and the dry forests of the Cerrado. But later on, in the 2010s, those hotspots of carbon loss were deeper in the Amazon and parts of the Congo Basin and those montane jungles in Southeast Asia.
The 20-year data set also revealed that more than two-thirds of the areas cleared for agriculture during the study period remained cleared in 2020.
“That’s a huge amount of area where, once you lose that carbon, you’re not returning it back,” Elsen said. “The fact that the cleared lands are staying cleared and the carbon is gone is definitely problematic.”
Molinario echoed that sentiment. But, he said, that statistic includes everything from forest that had been converted to agriculture nearly for two decades to land that had been cleared just a few years ago.
“What I would like to know is how many of the 2000 to 2005 clearings are still agriculture in 2020,” he added. “I wouldn’t assume that a farmer leaves the field that he just spent a half a year clearing … in just two years.”
Around the world, subsistence farmers employ shifting agriculture, clearing and usually burning the vegetation on a plot of land to prepare it for farming for a year or two. Then, farmers let the field lay fallow, often for years at a time, while moving on to cultivate another plot. The fallow period allows the land to recover and the forest to regrow — if it sits unused by humans for long enough.
But in some parts of the world, such as the Congo Basin, conflict, growing populations, and other pressures appear to have forced a shorter rotational cycle. That change means that forests haven’t been able to return as robustly as they once did. Molinario, who has worked on mapping forest loss in Central Africa, said there’s often more intensive farming with less time for the land to recover near the region’s larger towns, roads, mines and plantations.
“If we want to stop this issue, and we have to help those people living there to find [other ways] to increase their living standards … so they can they can better live with the forest,” said Zhenzhong Zeng, an associate professor and Earth systems scientists at SUSTech and a co-author of the study.
The fact that an area remains cleared of forest may indicate that the agriculture is more “intense” than it once was, said Alan Ziegler, a professor in fisheries and aquatic resources at Thailand’s Mae Jo University and a co-author of the study. In the Amazon and Southeast Asia, that can often mean industrial-scale agriculture or livestock ranching.
Feng said the team’s study serves as a warning that more effort needs to be put into protecting forests. The accelerating forest carbon loss uncovered by the study demonstrates that forest loss has not been reversed or even halted, the authors write. In 2020, the world missed a key deadline to halve rates of deforestation, a key goal of the 2014 New York Declaration on Forests.
This type of evidence also suggests global climate goals may be slipping out of reach, such as the effort to keep global warming under 1.5° Celsius (2.7° Fahrenheit) above pre-industrial levels. Scientists say a rise of 1.5°C or perhaps 2°C (3.6°F) could lead to dangerous and potentially irreversible impacts as a result of warming, triggered by sea-level rise, increasing drought and intensifying storms. World leaders committed to keeping warming to under 2°C in the 2015 Paris climate change agreement, and they reaffirmed the pledge, along with promised cuts in deforestation by 2030, at the 2021 U.N. climate conference in Glasgow.
Ziegler said the changes at these high-level meetings aren’t translating into action that will address the problem.
“We get together and shake hands, we make a pact, and then it really doesn’t make a change,” he said.
Forests play “a huge role in our ability to fight climate change” because of the massive amount of carbon they emit when they’re degraded or cleared, Elsen said. “This increasing acceleration of forest loss goes right in the face of a lot of the national commitments to help [stop] emissions.”
This study, however, does provide pathways to stem carbon emissions, the authors say, notably through forest protection and restoration.
“We know that just because we’re seeing a lot of deforestation … doesn’t mean that actions can’t be taken to restore healthy forests and restore some of that carbon,” Elsen said. “It does take time, but it is something that we should be investing in.”
Banner image: A researcher measures tree diameters during tropical peat swamp forest carbon monitoring in Central Kalimantan province, Indonesia. Image by Sigit Deni Sasmito/CIFOR via Flickr (CC BY-NC-ND 2.0).
John Cannon is a staff features writer with Mongabay. Find him on Twitter: @johnccannon
Citations:
Feng, Y., Zeng, Z., Searchinger, T. D., Ziegler, A. D., Wu, J., Wang, D., … Zheng, C. (2022). Doubling of annual forest carbon loss over the tropics during the early twenty-first century. Nature Sustainability. doi:10.1038/s41893-022-00854-3
Feng, Y., Ziegler, A. D., Elsen, P. R., Liu, Y., He, X., Spracklen, D. V., … Zeng, Z. (2021). Upward expansion and acceleration of forest clearance in the mountains of Southeast Asia. Nature Sustainability, 4(10), 892-899. doi:10.1038/s41893-021-00738-y
Hansen, M. C., Potapov, P. V., Moore, R., Hancher, M., Turubanova, S. A., Tyukavina, A., … Townshend, J. R. (2013). High-resolution global maps of 21st-century forest cover change. Science, 342(6160), 850-853. doi:10.1126/science.1244693
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