The North Country region is important for carbon sequestration because of its vast forests, wetlands, and relatively intact soils, however climate change disrupts this key ecosystem service. Increased rainfall and more frequent flooding impact aquatic ecosystems, soil health, wetland function, and forest health, affecting the ability of these ecosystems to sequester carbon. Warmer winters and shorter snow seasons decrease biodiversity through the alteration of habitats for species like alpine plants, boreal birds, moose, snowshoe hare, and brook trout, which depend on cold climates to thrive. Warmer temperatures lead to the spread of invasive species and pests, such as ticks and hemlock woolly adelgid, that threaten native plants, animals, and humans.
Check out the full report to read more about the efforts specific organizations in the North Country are undertaking to tackle these issues and the solutions proposed by listening session participants.
The unpredictability of seasonal weather patterns has caused economic disruption across various sectors, particularly tourism, agriculture, and forestry. In healthcare, emergency rooms anecdotally report an increase in cases of heat stroke and ice-related injuries due more erratic freeze-thaw cycles. Lack of seasonal predictability also affects the North Country cultural identity as residents not only take pride in their cold hardiness, but also celebrate popular winter festivals in communities throughout the region, and engage in winter cultural and recreational activities with generational significance.
The North Country is globally unique because it has both working and protected forests making up the landscape. Both types of forest lands have carbon sequestration as well as economic value, whether as part of the forest products industry, incentive programs like the Family Forest Carbon Program of the American Forest Foundation and The Nature Conservancy, or as part of the constitutionally protected Forest Preserve. The public forests making up the Forest Preserve offer long-term carbon storage potential; there is still room for substantial carbon sequestration as much of the Forest Preserve is relatively young at around 125 years old. The diversity of forest types allows for mixed economic use, enjoyment, and cultural importance, as well as supporting state climate initiatives.
In addition to public forest lands and working private forests, there are millions of acres of privately owned, non-commercial forestland across the state that are currently underutilized for conservation. Forests in Northern New York are experiencing change, with overall forest cover increasing even as property becomes more fragmented due to smaller parcel sizes and rising demand for second homes. This parcelization trend contributes to an expanded human footprint and reduced opportunity for agricultural land preservation. Some ACORN participants suggested that if new forest tax laws were designed to incentivize long-term carbon storage, in addition to current programs like 480 and 480A that require timber harvesting to trigger a tax incentive, it could unlock major climate benefits while supporting landowners and rural economies.
Invasive species were less of a topic in communities at a greater distance outside the Adirondack Park. Perhaps this is because invasives have been endemic for so many decades that it’s hard to recall prior intact ecosystems. In the higher elevations of the Adirondacks, groups did bring up invasives, but not to a great extent, perhaps because they still have relatively intact ecosystems. But in Warren and Washington County, invasive plants, fish, insects, and pathogens were a topic on nearly everyone’s mind, no matter their sector. This may be because Warren County is at the forefront of the recent range expansion for so many invasive species that have moved north in the last 15 years and residents and visitors can see the change happening before their eyes.
The Adirondack High Peaks are home to fragile alpine zone ecosystems, where rare plants adapted to cold, harsh conditions and strong winds have no other habitat to migrate to as temperatures rise and conditions change with a changing climate. In addition, warmer weather, changing snowpack, and more intense storms are causing soil erosion and allowing lower-elevation species to encroach on these sensitive habitats. Because alpine zones cover such a small area and are slow to recover from disturbance, even minor climate impacts can have outsized effects, putting these ecosystems at serious risk.
Climate change is already impacting water quality in the North Country in visible and measurable ways. Warmer temperatures are stressing cold-water fish like brook and lake trout, altering ice cover patterns, and triggering longer aquatic growing seasons, which increase the risk of harmful algal blooms and low-oxygen conditions. Water holds cultural, emotional, and economic value in the region, driving tourism, property values, the arts, and overall quality of life. However, early warning signs like changing water color, shifting thermoclines, and rising phosphorus levels point to growing stress on freshwater systems. Additionally, increased freeze-thaw cycles and storm-driven runoff are leading to higher road salt contamination, with some of the worst chloride levels in the state appearing in iconic lakes like Lake George.
Wetlands, particularly peatlands, sequester carbon through the accumulation of organic matter. Wetland functions are powered by water: where it comes from and the way it moves in and out of the wetland system. When wetland hydrology is disrupted, the wetland’s ability to provide essential services is also disrupted.
Wetlands offer major benefits that support both people and nature. They help control flooding, clean pollutants from water, recharge drinking water supplies, and support stormwater systems and sewer treatment. Wetlands are also rich in biodiversity, provide important fisheries habitat, and hold cultural and ecological value for Indigenous communities. Different types of wetlands serve different roles. Bogs, one type of peat-accumulating wetland, are closed systems that store large amounts of carbon and support unique plant species. Fens, which have seasonal water flow, are more diverse than bogs, and also store carbon. Wetlands with a higher proportion of underlying mineral soil don’t build up as much carbon due to regular flushing. The North Country region is the southern end of a massive peatland ecosystem that stretches into Canada, making this a key area for studying how peatlands might respond to climate change in the future.
New York State is studying wetlands more closely to better understand how they fit into the state’s climate strategy. A current effort through Cornell University is sampling wetlands and small ponds across the state to examine how much carbon these systems have stored in their soils over time. This work, which includes analyzing soil cores to estimate past carbon sequestration, will help determine whether NY’s wetlands are acting as carbon sinks or sources. The hope is that these findings will guide better planning for where roads cross wetlands, and help support culvert upgrades and hydrologic restoration. Wetlands naturally provide nature-based services that would cost billions to replicate with manmade infrastructure, making their protection and restoration a smart investment for NY’s future.