In mid-July 2016, satellites observed dense smoke over north-central Russia. Many of the fires appeared in the tundra-taiga interface, where boreal forests give way to low-lying vegetation and permafrost.
“It is not a sharp line,” said Bruce Forbes, a researcher at the University of Lapland. “Also, there can be ancient peat deposits near the surface to provide fuel in some places.”
These natural-color images were acquired by the Moderate Resolution Imaging Spectroradiometer (MODIS) on NASA’s Aqua satellite on July 19, 2016. The smoke grew denser as the fires proliferated. Red outlines show hot spots, indicating high surface temperatures often caused by fire.
Fires in the Yamalo-Nenets Autonomous District (top-left) also stand out on the most recent global fire anomaly map for 2016. The flames burn north of the tree line (in the tundra, where low temperatures and a short growing season limit tree growth). Here, peat moss thrives, and snow blankets the ground for much of the year. The first flurries typically fall in early September, at the end of fire season. The tundra is an important carbon sink, storing greenhouse gases in its soils. But the tundra is vulnerable to rising global temperatures, which dry out peat and turn it into prime kindling for wildfire. Fires in the far north, particularly in peatlands, produce huge quantities of carbon dioxide and methane, further fueling global warming.
Because of its vast scale and remote locale, the area poses challenges to field research and makes satellite data particularly valuable to researchers, noted Jessica McCarty-Kern, a scientist at the Michigan Tech Research Institute.
“In order to know what’s going on in the entire Arctic, you can’t leave out Russia, because Russia is one ninth of world’s landmasses,“ said McCarty-Kern. Russia spans a much larger Arctic area than Alaska, Canada’s Nunavut and Northwest Territories.
Fires hinder the ecosystem’s ability to hold carbon. The blaze produces huge quantities of CO2 and methane (a potent greenhouse gas) into the air. Instead of holding carbon, the ground releases it, further warming the earth.