The southern Appalachian spruce–fir forest is an ecoregion of the temperate coniferous forest biome, a type of montane coniferous forest that grows in the highest elevations in the southern Appalachian Mountains of the eastern United States. The ecoregion is the highest and coldest forest type in the southern Appalachian range, thriving in elevations above 5,500 feet (1,700 m) where the climate is too harsh to support the broad-leaved hardwood forest that dominates the region's lower elevations. A relict of the last Ice Age, this forest type covers just over 100 square miles (260 km2) and is considered to be among the most endangered ecosystems in the United States. Southern spruce–fir stands consist primarily of two needle-leaved evergreen species—the red spruce and the Fraser fir, nicknamed the "he-balsam" and "she-balsam," respectively. Regional entities sometimes refer to the southern spruce–fir forest as the "Canadian" or "boreal" forest because of its resemblance to the boreal forest of Canada. While southern spruce–fir forests are similar to the boreal forests and are home to many plant and animal species that are more common at northern latitudes, the southern spruce–fir is nevertheless a disjunct and unique ecosystem. Over the past two centuries, the southern spruce–fir stands have been decimated by logging, pollution, and an infestation of invasive insects. The southern spruce–fir forest is home to an endangered species, the spruce–fir moss spider, and several threatened species. While red spruce is common throughout North America, the Fraser fir—a relative of the balsam fir—is found only in the spruce–fir stands of southern Appalachia. In the second half of the 20th century, nearly all of the mature Fraser firs were killed off by the balsam woolly adelgid—a parasite introduced from Europe around 1900.
Occurrence
The southern Appalachian spruce–fir forest consists of several stands covering a combined area of between 60,000 and 70,000 acres (24,000 and 28,000 ha), although less conservative estimates have placed the forest's coverage at around 90,000 acres (36,000 ha). The largest southern spruce–fir stand is located in the higher elevations of the Great Smoky Mountains on the Tennessee-North Carolina border, stretching from roughly Kuwohi in the west to Mount Guyot in the east. Another significant spruce–fir stand is found atop the Black Mountains, and includes a large stand atop Mount Mitchell. Other significant stands are found in the Great Balsam Mountains (in southern North Carolina) and the Plott Balsams (between the Great Balsams and the Great Smokies). The Great Craggy Mountains and Mount Pisgah contain stands of red spruce but lack Fraser firs. Further north, southern spruce–fir forests coat the upper elevations of Roan Mountain, particularly the western part of the mountain between Roan High Knob and Roan High Bluff, and a smaller stand covers part of nearby Grandfather Mountain. The northernmost southern spruce–fir stand of note is found atop Mount Rogers and adjacent summits in Southwest Virginia. Smaller pockets of spruce forest have been identified in the higher elevations of West Virginia, although these are devoid of Fraser firs and are typically considered disjunct from the highland spruce–fir community. Roughly 95 percent of existing southern spruce–fir stands are owned by federal and state entities, with the remaining 5 percent privately owned. Approximately 85 percent of southern spruce–fir stands are found on National Park Service lands, namely in the Great Smoky Mountains National Park and in the Blue Ridge Parkway corridor, or on state-owned lands, such as at Mount Mitchell State Park or Grayson Highlands State Park. The remaining 10 percent of publicly owned southern spruce–fir stands are located on lands controlled by the United States Forest Service, namely the Pisgah National Forest in North Carolina, the Cherokee National Forest in Tennessee, and the Jefferson National Forest in Virginia.
Ecology
Climate
Southern Appalachian spruce–fir zones are on average much cooler than their surrounding valleys. Winter temperatures can reach as low as −30 °F (−34 °C) and can feel much colder if wind chill is taken into account. Strong thunderstorms and heavy rain showers are not uncommon in summertime, and spruce–fir zones are draped in clouds up to 25% of the time. They represent the southernmost extent of the humid continental climate in North America. Being atop mountain summits or ridgecrests, southern spruce–fir forests are often subjected to hurricane-force winds, the strongest of which have been recorded at 175 miles (282 km) per hour. Spruce–fir forest floors are often littered with blowdowns, and roads and trails that traverse spruce–fir forests require frequent maintenance to remove downed trees and branches.
Flora
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