The climate is changing faster in northern latitudes than the rest of the globe, intensifying wildfire regimes across the boreal landscape.

Boreal forests punch above their weight when it comes to carbon storage—they make up a third of global forests, but store roughly two thirds of global forest carbon, mainly in the organic matter in their soils. However, these important carbon stores are at risk in a changing climate.

Longer fire seasons, more intense fire weather, and increased lightning ignitions are intensifying fire regimes in the north. The resulting increase in fires, their severity, and the area burned directly contributes to larger amounts of carbon being emitted into our atmosphere. However, boreal fire emissions are largely missing from the climate models that inform the IPCC and global carbon budgets.

How will boreal fire regimes continue to evolve, how will these changes impact greenhouse gas emissions and our global climate, and is there anything we can do about it?

Our Work

Impact

While some climate models include boreal fire, they do not capture the emissions generated when fire burns soil organic matter or thaws permafrost. Our work aims to elevate and socialize these emissions as the global climate threat that they are, and to quantify how their release will impact our ability to meet climate targets.

Our research showing fire management to be a cost-effective natural climate solution has received attention because of its potential impact on carbon budgets. Our ultimate aim is to increase funding for boreal fire management agencies and operationalize carbon and permafrost protection from fire in the US (Alaska) and Canada. Our work on fire management and self-regulation can also help inform fire management agencies’ practices with improved tools and understanding.

Methane is second only to carbon dioxide (CO2) in its contribution to human-induced climate change, thanks to its global warming potential—34x greater than CO2.

However, we understand very little about methane flux in forests, the processes and feedbacks that drive it, and how methane emissions or uptake will evolve with a changing climate.

Our Work

At the Howland Research Forest, ME, we are taking on this priority for biological research and improving methane flux models. Our innovative, multi-scale, and cross-disciplinary study is identifying the conditions and mechanisms driving methane sink/source activity across soil moisture gradients in northern forests.

Led by Woodwell Climate Research Center, in collaboration with the University of Maine, Emory University, Arizona State University, San Diego State University, and the USDA Forest Service, this research uses new DNA/RNA sequencing techniques that allow us to study microbial traits. Measuring these traits across different environmental conditions ultimately helps us learn how microbes’ sequestration of methane in sub-boreal forests may be offsetting methane emitters globally, and how this may change under future climate conditions. The Howland Research Forest serves as a case study to identify drivers and functional relationships across wet to dry soils, and from soils to canopy.

This conceptual diagram shows fluxes of methane (CH4) between wetland and dry upland areas within a sub-boreal forest. Soil micro-organisms produce methane under wet conditions, while others consume methane under dry conditions. The eddy covariance tower shown on the right of the diagram measures the net exchange of methane to determine if the area is a source (release) or sink (uptake) of methane.

Our work at Howland Forest has three main components:

  1. Belowground (soils) to aboveground (trees) processes: Using both field and lab experiments, we are measuring methane fluxes, microbial traits, and environmental conditions below and above ground in the forest. This will help us identify the role of microbial processes and physical drivers in regulating methane flux, and we can compare these measurements to those taken by the forest’s eddy flux tower to better describe the overall movement of methane within the landscape.
  2. Improving process-based ecosystem models: Our field and lab observations will ultimately guide much-needed improvement of ecosystem models such as the Microbial Model for Methane Dynamics (M3D)-DAMM and Community Land Model-Microbe process models.
  3. Predictions across space and time: We will apply our laboratory and field data toward improving models that identify both seasonal and annual methane sink/source activity at Howland, from present to 2100.

Our Impact

Our study is providing new insights for carbon budgets into how methane uptake in northern forests may be offsetting methane emissions, as well as how these systems might shift to net emission under projections of increasing precipitation across the northeastern region of the United States. We are ensuring that this improved understanding reaches broad audiences through a range of activities:

  1. Global methane workshop (2024): We are hosting a three-day methane workshop at the UMaine campus and at Howland forest to promote co-production of knowledge, bringing together global experts in methane. Scientists from the Arctic to the Tropics will discuss how they can better integrate field-lab-model approaches to improve understanding of ecosystem gas exchange at field-to-global scales.
  2. Local outreach to high schools: Our team is coordinating “scientist in the classroom” outreach visits to local high schools, and inviting local Maine students and the public to an open house at the Howland Research Forest to learn about this research.
  3. Training the next generation of scientists: This project directly supports the cross-disciplinary training of 2 Postdocs, 2 Ph.D. students, and at least 8 undergraduate students, primarily from underrepresented groups. Interested students can reach out to Kathleen Savage.

Phenology Cam

Howland Research Forest is part of an international phenology camera network, hosted at Northern Arizona University. There are two cameras located at the Main tower site.

See the view from Howland Forest’s main tower.

See the view from Howland Forest’s north tower.

 

This project is supported by the National Science Foundation Division of Environmental Biology.

Site location: 59.85 N; -151.06 W (WGS1984)

Site name: Caribou Hills South

Description: This site is located on private land, 32 km (20 miles) NE of Homer, southern Kenai Peninsula, Alaska, on a natural grassland at ~1400 ft elevation (~425 m). The boreal forest in the Kenai Peninsula is transitioning to a grassland ecosystem due to changes in climate (drier and warmer) and bark spruce beetle attacks. This location has likely been a grassland since the last glaciation (~10,000 years ago). The meteorological station was installed in late November 2022 to allow for the collection of baseline meteorological and soil data representing an ecosystem type that has not received much attention in Alaska. Further, the region around Homer experiences large temperature, wind, and precipitation gradients that are not well quantified. The data is updated every hour. The plots represent raw data, i.e. it is not quality controlled. The Kenai Mountains in the background (south) reach up to 2000 m (~6000 ft) and when the weather is good you can see the Dixon and Portlock Glaciers. This data collection is made possible through a collaboration between the Water and Environmental Research Center at the University of Alaska Fairbanks and Woodwell Climate Research Center. If you want to learn more, please contact Anna Liljedahl (aliljedahl@woodwellclimate.org).

Data graphs: ine.uaf.edu/werc/projects/woodwell/caribouhillssouth.aspx