Deforestation may intensify global warming even more than previously predicted | AGÊNCIA FAPESP

Deforestation may intensify global warming even more than previously predicted Unless the clearing of tropical forests is halted, the mean global temperature could rise an extra 0.8 °C, even with cuts in emissions from fossil fuels, scientists warn in an article in Nature Communications (photo: GoAmazon)

Deforestation may intensify global warming even more than previously predicted

March 07, 2018

By Karina Toledo  |  Agência FAPESP – The global warming process may be even more intense than originally forecast unless deforestation can be halted, especially in the tropical regions.

This warning has been published in Nature Communications by an international group of scientists. The authors of the text include Brazilians Paulo Artaxo, a professor at the University of São Paulo’s Physics Institute (IF-USP), and Luciana Varanda Rizzo, a professor at the Federal University of São Paulo’s Environmental, Chemical & Pharmaceutical Science Institute (ICAQF-UNIFESP).

“If we go on destroying forests at the current pace – some 7,000 km² per year in the case of Amazonia – in three to four decades, we’ll have a massive accumulated loss. This will intensify global warming regardless of all efforts to reduce greenhouse gas emissions,” Artaxo told Agência FAPESP.

The findings of the study are based on computer modeling and forest measurements coordinated by Catherine Scott, a researcher at the University of Leeds in the United Kingdom.

Having spent years collecting data on the functioning of tropical and temperate forests, the gases emitted by vegetation, and their impact on climate regulation, the group succeeded in mathematically reproducing the planet’s current atmospheric conditions, including levels of aerosols, anthropogenic and biogenic volatile organic compounds (VOCs), ozone, carbon dioxide, methane, and all the other factors that influence global temperature, such as surface albedo. 

Albedo is a measure of the reflectivity of a surface. The albedo effect when applied to Earth is a measure of how much of the Sun’s energy is reflected back into space. The fraction absorbed changes according to the type of surface.

The researchers used a numerical model of the atmosphere developed by the Met Office, the UK's national meteorological service.

“After adjusting the model to reproduce the current conditions of Earth’s atmosphere and the rise in surface temperatures that has occurred since 1850, we ran a simulation in which the same scenario was maintained but all forests were eliminated,” Artaxo said. “The result was a significant rise of 0.8 °C in mean temperature. In other words, today the planet would be almost 1 °C warmer on average if there were no more forests.”

The study also showed that the difference observed in the simulations was due mainly to emissions of biogenic VOCs from tropical forests.

“When biogenic VOCs are oxidized, they give rise to aerosol particles that cool the climate by reflecting part of the Sun’s radiation back into space,” Artaxo said. “Deforestation means no biogenic VOCs, no cooling, and hence future warming. This effect was not taken into account in previous modeling exercises.”

Temperate forests produce different VOCs with less capacity to give rise to these cooling particles, he added. 

Data collection

The article notes that forests cover almost a third of the planet’s land area, far less than before human intervention began. Huge swathes of forest in Europe, Asia, Africa and the Americas have been cleared. 

Collection of data on the functioning of the Amazon rainforest began in 2009 as part of two Thematic Projects supported by FAPESP and with Artaxo as principal investigator: “GoAmazon: interactions of the urban plume of Manaus with biogenic forest emissions in Amazonia”, and “AEROCLIMA: direct and indirect effects of aerosols on climate in Amazonia and Pantanal”.

The data on temperate forests was obtained in Sweden, Finland and Russia. Collection was coordinated by Erik Swietlicki, a professor at Lund University in Sweden.

“It’s important to note that the article doesn’t address the direct and immediate impact of forest burning, such as emissions of black carbon [considered a major driver of global warming owing to its high capacity for absorbing solar radiation]. This impact exists, but it lasts only a few weeks. The article focuses on the long-term impact on temperature variation,” Artaxo said.

Deforestation, he stressed, affects the amount of aerosols and ozone in the atmosphere definitively, changing the atmosphere’s entire radiative balance.

“The urgent need to keep the world’s forests standing is even clearer in light of this study. It’s urgent not only to stop their destruction but also to develop large-scale reforestation policies, especially for tropical regions. Otherwise, the effort to reduce greenhouse gas emissions from fossil fuels won’t make much difference,” Artaxo said.

The article “Impact on short-lived climate forcers increases projected warming due to deforestation” (doi:10.1038/s41467-017-02412-4) by C. E. Scott, S. A. Monks, D. V. Spracklen, S. R. Arnold, P. M. Forster, A. Rap, M. Äijälä, P. Artaxo, K. S. Carslaw, M. P. Chipperfield, M. Ehn, S. Gilardoni, L. Heikkinen, M. Kulmala, T. Petäjä, C. L. S. Reddington, L. V. Rizzo, E. Swietlicki, E. Vignati and C. Wilson can be read at:



Agência FAPESP licenses news reports under Creative Commons license CC-BY-NC-ND so that they can be republished free of charge and in a straightforward manner by other digital media or by print media. The name of the author or reporter (when applied) must be cited, as must the source (Agência FAPESP). Using the button HTML below ensures compliance with the rules described in Agência FAPESP’s Digital Content Republication Policy.

Topics most popular