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Global Warming’s New Threat: Arctic Permafrost’s Carbon Bomb

Recent Dartmouth research underscores the significant influence of Arctic permafrost on the formation of northernmost rivers and highlights the risks of substantial carbon release due to climate change-induced thawing. By analyzing thousands of watersheds, the study reveals the unique characteristics of Arctic river valleys and stresses the importance of understanding these landscapes in the face of global warming. Credit:

As the Arctic warms, the growth of rivers could release carbon emissions equivalent to those of millions of vehicles.

Recent findings from Dartmouth reveal groundbreaking evidence that the Arctic’s permafrost significantly influences the region’s river systems. This study, published in the Proceedings of the National Academy of Sciences, highlights how permafrost—a dense layer of soil that remains frozen for at least two years—causes rivers in the Arctic to flow through narrower and shallower valleys compared to their southern counterparts.

But permafrost also is an increasingly fragile reservoir of vast amounts of carbon. As climate change weakens Arctic permafrost, the researchers calculate that every 1.8 degrees FahrenheitThe Fahrenheit scale is a temperature scale, named after the German physicist Daniel Gabriel Fahrenheit and based on one he proposed in 1724. In the Fahrenheit temperature scale, the freezing point of water freezes is 32 °F and water boils at 212 °F, a 180 °F separation, as defined at sea level and standard atmospheric pressure. ” data-gt-translate-attributes=”[{“attribute”:”data-cmtooltip”, “format”:”html”}]” tabindex=”0″ role=”link”>Fahrenheit (1 degree CelsiusThe Celsius scale, also known as the centigrade scale, is a temperature scale named after the Swedish astronomer Anders Celsius. In the Celsius scale, 0 °C is the freezing point of water and 100 °C is the boiling point of water at 1 atm pressure.” data-gt-translate-attributes=”[{“attribute”:”data-cmtooltip”, “format”:”html”}]” tabindex=”0″ role=”link”>Celsius) of global warming could release as much carbon as 35 million cars emit in a year as polar waterways expand and churn up the thawing soil.

Landscape Dynamics and Research Motivation

“The whole surface of the Earth is in a tug of a war between processes such as hillslopes that smooth the landscape and forces like rivers that carve them up,” said first author Joanmarie Del Vecchio, who led the study as a Neukom Postdoctoral Fellow at Dartmouth with her advisers and study co-authors Marisa Palucis, an assistant professor of earth sciences, and engineering professor Colin Meyer.

“We understand the physics on a fundamental level, but when things start freezing and thawing, it’s hard to predict which side is going to win,” Del Vecchio said. “If hillslopes win, they’re going to bury all that carbon trapped in the soil. But if things get warm and suddenly river channels start to win, we’re going to see a large amount of carbon get released into the atmosphere. That will likely create this warming feedback loop that leads to the release of more greenhouse gases.”

Del Vecchio

Dartmouth researchers set out to understand why Arctic watersheds tend to have less river area than watersheds in warmer climates. First author Joanmarie Del Vecchio (pictured) conceived of the study while conducting fieldwork in Alaska after she hiked uphill from her riverside worksite and beheld a vista of sheer mountain slopes unbroken by rivers or streams. Credit: Mulu Fratkin

The researchers set out to understand why Arctic watersheds — the total drainage area of a river and its connected waterways — tend to have less river area than watersheds in warmer climates, which can have extensive tributaries that spread over the landscape. Del Vecchio, now a visiting scholar at Dartmouth and an assistant professor at the College of William and Mary, conceived of the study in 2019 while conducting fieldwork in Alaska. She hiked uphill from her riverside worksite and beheld a vista of sheer mountain slopes unbroken by rivers or streams.

It seemed like the hillslopes were winning and the channels were losing,” Del Vecchio said. “We wanted to test whether it was temperature shaping this landscape. We’re very lucky to have had the amount of surface and digital elevation data that’s been produced in the past few years. We couldn’t have done this study a few years ago.”

Study Findings and Analysis

The researchers examined the depth, topography, and soil conditions for more than 69,000 watersheds across the Northern Hemisphere — from just above the Tropic of Cancer to the North Pole — using satellite and climate data. They measured the percentage of land each river’s channel network occupies within its watershed, as well as the steepness of river valleys.

Forty-seven percent of the analyzed watersheds are shaped by permafrost. Compared to temperate watersheds, their river valleys are deeper and steeper, and about 20% less of their surrounding landscape is occupied by channels. These similarities are despite any differences in glacial history, background topographic steepness, annual precipitation, and other factors that would otherwise govern the push and pull of water and land, the researchers report. Arctic watersheds are shaped by the one thing they have in common — permafrost.

“Any way we sliced it, regions with larger, more plentiful river channels are warmer with a higher average temperature and less permafrost,” Del Vecchio said. “You need a lot more water to carve valleys in areas with permafrost.”

Permafrost’s power to limit the footprint of Arctic rivers also allows it to store vast amounts of carbon in the frozen earth, according to the study. To estimate the carbon that would be released from these watersheds due to climate change, the researchers combined the amount of carbon stored in permafrost with the soil erosion that would result as the ground thaws and is washed away as Arctic rivers spread.

Climate Change Impacts and Future Concerns

Research suggests that the Arctic has warmed by more than 3.6 degrees Fahrenheit (2 degrees Celsius) above pre-industrial levels, or roughly since 1850, Del Vecchio said. Scientists estimate that a gradual thawing of Artic permafrost could release between 22 billion and 432 billion tons of carbon dioxide by 2100 if current greenhouse gas emissions are reined in — and as much as 550 billion tons if they are not, she said. The International Energy Agency estimates that energy consumption in 2022 spewed more than 36 billion tons of carbon dioxide into the atmosphere, an all-time high.

The Arctic has been adapted to the cold for so long that scientists have little idea of how much, or how fast, carbon will be released if permafrost thaws on an accelerated timescale, said Palucis, whose research group uses the Arctic as a stand-in for MarsMars is the second smallest planet in our solar system and the fourth planet from the sun. It is a dusty, cold, desert world with a very thin atmosphere. Iron oxide is prevalent in Mars' surface resulting in its reddish color and its nickname "The Red Planet." Mars' name comes from the Roman god of war.” data-gt-translate-attributes=”[{“attribute”:”data-cmtooltip”, “format”:”html”}]” tabindex=”0″ role=”link”>Mars to study the Red Planet’s surface processes. “While the Arctic has experienced warming in the past, the scary thing is how rapidly it’s occurring now. The landscape must respond quickly and that can be traumatic,” she said.

Palucis recalled a research trip to the Arctic when she saw a chunk of bedrock the size of a small building break off from a cliff. The culprit of the cleaving was a small stream of water that had seeped into the rock and weakened it.

“This is a landscape that is adapted to colder conditions, so when you change it, even a small amount of water flowing through rock is sufficient to cause substantial change,” Palucis said.

“Our understanding of Arctic landscapes is more or less where we were with temperate landscapes 100 years ago,” she said. “This study is an important first step in showing that the models and theories we have for temperate watersheds just can’t be applied to polar regions. It’s a whole new set of doors to go through in terms of understanding these landscapes.”

Sediment cores collected from the Arctic have shown extensive soil runoff and carbon deposits roughly 10,000 years ago, suggesting a much warmer region than exists now, Del Vecchio said. Today, areas such as Pennsylvania and the Mid-Atlantic United States that are just south of the farthest reach of the Ice Age glaciers portend the modern Arctic’s future.

“We have some evidence from the past that a lot of sediment was released into the ocean when there was warming,” Del Vecchio said. “And now we have a snapshot from our paper showing the Arctic will get more water channels as it gets warmer. But none of that is the same as saying, ‘This is what happens when you take a cold landscape and turn up the temperature real fast.’ I don’t think we know how it will change.”

Reference: “Permafrost extent sets drainage density in the Arctic” by Joanmarie Del Vecchio, Marisa C. Palucis and Colin R. Meyer, 1 February 2024, Proceedings of the National Academy of Sciences.
DOI: 10.1073/pnas.2307072120

The study was funded by the National Science Foundation, the National Aeronautics and Space Administration, the Army Research Office, and Neukom Institute for Computational Science.

Source: SciTechDaily