Trees affect albedo rates of the earth’s surface. Albedo is defined by The Free Dictionary as: “The fraction of incident electromagnetic radiation reflected by a surface, especially of a celestial body.” An example of a high albedo surface is land covered with snow. Basically, more of the sun’s radiation is reflected with snow on the ground, resulting in less warming.
It is generally accepted and portrayed by general circulation models (GCM’s) that deforestation decreases the albedo rate of the land. Decreasing the albedo further contributes to the problem of equatorial warming. So a subversive way trees fight climate change is through increasing, or maintaining, albedo rates.
Tress can creates thick cloud cover, as famously portrayed in Amazon rainforest images. Deforestation can cause decreases in humidity and its’ associated clouds. This sets off many reactions that have varying effects on global climate change.