Satellites yield insight into not so permanent permafrost
Land-cover map of the Arctic covering 1500 km north to south to understand how thawing permafrost is changing the landscape. The map has been generated using information from the Copernicus Sentinel-1 and Sentinel-2 missions. Tones of yellow and beige show sparse vegetation, greens show tundra, purples show forest and reds show areas that have been disturbed by flooding or forest fires. Vegetation patterns alter snow re-distribution and therefore heat transfer in winter and fires can trigger permafrost thaw.
Credit: contains modified Copernicus Sentinel data, processed by ZAMG
Ice is without doubt one of the first casualties of climate change, but the effects of our warming world are not only limited to ice melting on Earth’s surface. Ground that has been frozen for thousands of years is also thawing, adding to the climate crisis and causing immediate problems for local communities.
In Earth’s cold regions, much of the sub-surface ground is frozen. Permafrost is frozen soil, rock or sediment—sometimes hundreds of metres thick. To be classified as permafrost, the ground has to have been frozen for at least two years, but much of the sub-surface ground in the polar regions has remained frozen since the last ice age.
Permafrost holds carbon-based remains of vegetation and animals that froze before decomposition could set in. Scientists estimate that the world’s permafrost holds almost double the amount of carbon than is currently in the atmosphere.
When permafrost warms and thaws, it releases methane and carbon dioxide, adding these greenhouse gases to the atmosphere and making global warming even worse.
With permafrost covering about a quarter of the northern hemisphere, extensive thawing could trigger a feedback loop that could potentially turn the Arctic from a carbon sink into a carbon source.
Thawing permafrost isn’t just releasing more greenhouse gasesinto air—it’s also changing the landscape and destabilising the ground, and so causing real practical problems for society.
Over 30 million people live in the permafrost zone, in towns that were built on firm ground. As the ground softens, the infrastructure that Arctic communities rely on is becoming increasingly unstable.
Determined by temperature, permafrost is an essential climate variable. Through ESA’s Climate Change Initiative, temperature data that have been collected over years are gathered to determine trends and to understand more about how permafrost fits into the climate system.
Traditionally, direct temperature observations are made through boreholes. However, the measurement network is rather sparse because of the obvious remoteness and logistical issues in the Arctic.
Therefore, other types of information that reflect change are needed to fill the vast gaps across the Arctic and other mountain regions.
Discussed at this week’s Living Planet Symposium, satellites are an important part of monitoring permafrost, albeit indirectly, from space.
Annett Bartsch, the founder and managing director of b.geos, explained, “We can’t monitor permafrost as such from space. Although it’s a bit complicated, we can, however, use a lot of different types of satellite data along with in situ measurements and modelling to put together a picture of what is happening.
“Through an ESA project called Glob Permafrost, we use images captured by the Copernicus Sentinel-2 mission, for example, which give us a camera-like view of how the land surface is slumping and eroding because of thawing permafrost. The Copernicus Sentinel-1 radar mission, on the other hand gives us valuable information on widespread changes in topography.
“Missions carrying thermal sensors such as Copernicus Sentinel-3 can provide information about the changes in the temperature of Earth’s surface.
“And, we can use information on snow conditions and land coveras a proxy for soil properties. Both snow and soil regulate heat transfer, so they determine the actual impact of increasing air temperature on the frozen soil beneath.”