Multi-decadal year-round CO2 and CH4 fluxes to understand long-term impact of climate change on the Arctic carbon balance

Organic carbon in northern soils is more than double the current atmospheric pool. An increasing fraction of this organic carbon is vulnerable to conversion to carbon dioxide and methane. Temperatures in far northern latitudes have increased by 0.6 °C in the last 30 years, which is twice the global average with the largest increase in the non-summer seasons. This increase has been linked to increased atmospheric concentration of greenhouse gas fluxes in high latitude wetlands but the drivers of this renewed growth are still largely uncertain. This project establishes long-term, year-round field observations to better understand the controls on greenhouse gas (GHG) emissions from the Arctic at time scales that will encompass climate change and variability.

Participants Involved in This Project

Holli outdoors

Holli Grant | Educator Fellow

Lake Worth ISD | Lake Worth, Texas
Macall in front of snow

Macall Hock | Researcher Fellow

San Diego State University | San Diego, CA

From the Blog

The team using the conductivity, temperature and depth tool on board the ship
A Day in the Life
The US academic research vessel RV Neil Armstrong departed from Nuuk, Greenland in early October. On the first leg of our journey, the science team’s initial purpose was to collect water samples and previously deployed instruments along a line of moorings at the southern entrance to Baffin Bay, a gateway between the Arctic and the north Atlantic. This line stretches from Sisimiut, on the west side of Greenland, to just off Cape Dyer, near the Canadian coast. 
The Power of Collaboration
Our plane glides through the Endicott Mountains of the Brooks Range as we make our final descent into Anaqtuuvak. Accessible only by plane, Anaktuvuk Pass (“the place of caribou droppings”) is located 250 miles northwest of Fairbanks and is home to the only community of inland Iñupiat, Nunamiut, people [1]. Below, icy blue glaciers feed into a winding network of streams that snake through dense, green tundra and low-lying willows that line the banks of the Anaktuvuk River. From the air, the tundra is a verdant forest, but once on the ground the trees and shrubbery are no taller than 5-6 feet. The village stands out like a colorful flower within the greenery, blooming into view as we enter the valley. In Anaktuvuk, the roots of plants and people alike extend down into permafrost, the lifeblood of the ecosystem and holder of history. 
Polar STEAM Vlog on YouTube
Connecting to the Classroom
In July 2024 I had the opportunity to visit Amy in person in Arizona.  In the vlog of my trip, I share pictures of the work one of Amy’s colleagues is doing on a telescope that is going in a hot air balloon in Antarctica, we visit Kitt Peak Observatory, which is built on the tribal land of the Tohono Odham nation, and then Amy’s lab at the University of Arizona.  You will also hear snippets of the songs I wrote for our Polar STEAM resource assignment.
Erika wearing a puffy jacket and holding up her hands in front of shelves of ice cores.
The Power of Collaboration
As a high school science teacher, I’m always looking for ways to inspire my students with real-world science and deepen their understanding of our planet. The PolarSTEAM Educator Fellowship has been an extraordinary opportunity to merge my passion for polar environments with my teaching. Through this year-long virtual collaboration with T.J. Fudge, a research scientist at the University of Washington, I’ve been immersed in cutting-edge research on ice cores, allowing me to bring current polar science research to my students.
Seven people sit up in sleeping bags in front of a building
A Day in the Life
The Juneau Icefield is a group of interconnected glaciers just north of Juneau, Alaska that extends into British Columbia, Canada and covers an area the size of Rhode Island. Maybe you’ve heard of the Mendenhall Glacier? It is part of the Juneau Icefield! The Juneau Icefield Research Program (JIRP) has been collecting data on the icefield since 1948.