Deforestation drives fire risk in Borneo amid a warming climate, study finds - Mongabay

Annual peatland fires in Indonesia affect ecology, air quality, nutrient distribution of the soil, and human health. A modeling study finds that under current climate change projections and with rapid deforestation in Borneo, fire risk increases by the end of the century. The findings show that deforestation is a significant factor in fire risk. While local governments can’t control global climate change, they work to stem forest loss and invest in reforestation of tropical forests and revitalization of peatlands to mitigate fire risks in the future, researchers say.

The dry season of 2015 was a devastating one for Indonesia, with around 100,000 fires engulfing thousands of hectares of tropical rainforests and carbon-rich peatlands on the islands of Sumatra, Borneo and New Guinea. The infernos, strengthened by dry weather caused by El Niño, raged for months, in the process emitting more carbon dioxide than a year’s worth of U.S. economic activity. The haze spread so far it threatened public health not just in Indonesia, but also in Singapore, Malaysia and Thailand, leading an Indonesian government agency to label the fires a “crime against humanity.”

 

While the 2015 fires were particularly severe, reports of such tropical forest fires in Indonesia, especially Borneo, have hit headlines almost every year for decades. A recent study predicts that as climate change worsens and deforestation intensifies in the region, the risk of forest fires will only continue to increase.

 

The study, published in the journal Environmental Research Letters, calculated the combined effect of climate change and deforestation on fire risk in Borneo, and found that while high levels of CO2 in the atmosphere increase fire risk, deforestation, which causes the dry conditions that fuel the fires, significantly contributes to it.

 

Growing risk of fires

 

As the planet warms, wildfires have become increasingly frequent and intense across the world. Tropical forests, which greatly impact the local climate, temperature and rainfall, cover more than half of Kalimantan, the Indonesian part of Borneo. In the past few decades, about a third of these tropical forests have been cut down to make way for oil palm and rubber plantations, often using slash-and-burn practices that can spark out-of-control fires. The draining of perennially water-bogged peatlands has made conditions on the ground even more conducive for fires.

 

While previous studies have established the role of climate change and deforestation in increased fire risk, this study projects their combined effects into the future. “We use climate models with as fine a spatial scale as we can to actually make these predictions to see where the risk of fire increases,” says study author Frank van Veen from the University of Exeter, U.K., who also leads Kalimantan Lestari, an interdisciplinary project focused on building resilience against drought and peatland fires in the province of Central Kalimantan.

 

The researchers simulated changes to Borneo’s climate with elevated levels of CO2 in the atmosphere in the business-as-usual scenario (also known as RCP8.5), and intensified deforestation where tree cover declined from 72% in 2000 to 0% by the end of the century. Then, they calculated the combined effect of elevated CO2 levels and complete deforestation to estimate variations in rainfall, temperature, humidity and winds — all of which determine fire risk.

 

The modeling indicates that around peatlands, which are at lower elevations, deforestation increases the peak level of fire risk during the dry season (June, July and August) more so than elevated atmospheric CO2 does. However, climate change increases the mean fire risk during this period. At high elevations, above 500 meters (1,640 feet), deforestation accounts for 53% of the projected annual temperature increase for the 21st century. The models also predict an increase in extreme dry and wet years, rather than just an increase in the average temperature.

 

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