The bombshell research was led by Christopher A. Williams, an environmental scientist and professor in Clark University’s Graduate School of Geography.

The peer-reviewed study will likely have far-reaching implications for policy and land management efforts across the US and beyond.

Using state-of-the-art satellite remote sensing, as opposed to computer models as was the case in many previous studies, Williams and his team examined what uses various deforested areas were repurposed for (urban, agricultural, grassland etc.) and quantified how much biomass carbon was released into the atmosphere as a result.

They then calculated how much additional sunlight would be reflected back out into space as a result, depending on the particular change in landscape.

The research indicates that the solution to planetary warming caused by climate change may not be as straightforward as just planting more trees.

Forests absorb carbon dioxide, store it in wood and soil and alleviate the greenhouse gas burden on the atmosphere.

However, forests also tend to be quite dark, and absorb and retain more sunlight, and by extension heat, in a process called the “albedo effect”.

“We found that in some parts of the country like the Intermountain West, more forest actually leads to a hotter planet when we consider the full climate impacts from both carbon and albedo effects,” said Professor Williams.

Striking a balance between this effect and forests’ carbon capture and storage capabilities is important to forming coherent and effective public environmental policy in the US and beyond.

For one quarter of the US, forest loss contributed to a net cooling effect, as the previous tree density created an albedo effect which outweighed the trees’ carbon absorption.