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Deforestation in the tropics affects climate around the world, study finds

A worldwide study on tropical deforestation reveals how far-reaching its impact can be.  Robert McSweeney explains the findings of the study.


'THE effects of tropical deforestation on climate go well beyond carbon,' says Professor Deborah Lawrence, '[it] causes warming locally, regionally and globally, and it changes rainfall by altering the movement of heat and water.'

These are the conclusions of a worldwide study into the deforestation of tropical rainforests, which shows that cutting down trees can have immediate impacts on the climate and put agricultural productivity at risk.

Rainforests are more than just a carbon store

Deforestation and land use change account for approximately11% of global carbon dioxide emissions. But the new research finds that cutting down trees doesn't only affect the carbon they lock up.

The research, published in Nature Climate Change, reviews academic studies on deforestation of tropical rainforests in the Amazon basin, Central Africa and Southeast Asia. Many of the studies use climate models to simulate what happens if you remove these forests completely, and they suggest that deforestation in the tropics can affect the climate on the other side of the world.

The models suggest deforestation in the Amazon, for example, can reduce rainfall over the US Midwest and even in northeast China. Deforestation in Central Africa can cause a drop in rainfall in Southern Europe, and loss of trees in Southeast Asia can bring wetter conditions in Southern Europe and the Arabian Peninsula.

Lead author Lawrence tells the Carbon Brief website in an email: 'These are physical effects from removing trees that are not simply related to the loss of carbon dioxide stored inside them. Tropical deforestation results in immediate climate impacts independent of, and in addition to, its contribution to the greenhouse effect.'

Tropical deforestation is a global problem

So how does it work? How can cutting trees down in the Amazon affect rainfall in China?

First you have to bear in mind that rainforests cool the air above them by turning water from the soil into moisture in the air. Chop the trees down, and you remove the cooling effect from this additional moisture. The effect is so pronounced, the study finds, that if all the trees in the tropics were cut down, global temperature could increase by as much as 0.7 degrees.

With the trees gone the air warms up, creating large, rising masses of warm air. When these air masses hit the upper reaches of the atmosphere, they create ripples called teleconnections that flow towards the mid- and higher latitudes.

Lawrence compares it to boiling water: 'Imagine steam rising off a pot of boiling water, hitting the ceiling in your kitchen and flowing outward, along the ceiling, out the door to your hallway.'

So these changes to the atmosphere in the tropics can flow out to the atmosphere of temperate regions and alter their climate, Lawrence says.

Worst-case scenario

It seems unlikely we'll ever cut down an entire rainforest. So why do scientists run these experiments? Lawrence explains: 'We want to understand just how important rainforests are to sustaining the life support system on earth, and we start with a worst-case scenario. Large-scale tropical deforestation is the outcome of business-as-usual economic development, it is the path we took in the US and Europe during the course of our development.'

Scientists also use more realistic scenarios, Lawrence says, which help identify potential tipping points if deforestation continues at current rates. For example, some studies show that clearing 30-50% of the Amazon would trigger a drop in rainfall that could cause a significant decline in how the rainforest functions as an ecosystem.

The study also looks at changes that have already happened as forests have been cleared. In Brazil, for example, the rainy season starts 11 days later in deforested areas, and scientists think that the loss of trees in Central Africa may have caused a more than 20% decline in rainfall from the Congo basin to the east coast.

Implications for agriculture

Scientists have also modelled the impact climate changes from deforestation could have on farming in the tropics.

Warmer and drier conditions caused by deforestation could put agricultural productivity at risk, the study finds. Yields of soy in the Amazon, for example, are projected to drop by up to 60% if more trees are cut down, and cattle production may not be viable in some areas as the quality of pasture declines. Adaptation measures might reduce the impact of these effects to some extent, of course.

Deforestation can also cause longer dry seasons and delays to the start of the rainy season, the study suggests. Because forests help moderate high daytime and low nighttime temperatures, cleared land is more susceptible to temperature extremes, which some crops may not tolerate.

Limiting deforestation is therefore important for farming as well as tackling climate change, Lawrence argues: 'Agriculture and forestry need to be considered together. Maintaining large tracts of tropical forest is essential for maintaining a climate that sustains tropical agriculture. Forest conservation is an essential aspect of planning for agricultural development.'

And alongside climate change, cutting down trees will make growing crops and raising livestock even harder: 'We are already anticipating worldwide challenges to food security because of what we are doing to the atmosphere. Now we have to worry about additional climate challenges because of what we are doing to the surface of the earth.'                       

Robert McSweeney covers climate science for the Carbon Brief website (www.carbonbrief.org), from which this article is reproduced. He holds an MEng in Mechanical Engineering from the University of Warwick and an MSc in Climate Change from the University of East Anglia in the UK. He previously spent seven years working on climate change projects at the consultancy firm Atkins.

*Third World Resurgence No. 292, December 2014, pp 28-29


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