FIRE AND FOREST HISTORY AT MOUNT RUSHMORE

Ecological Applications - Tập 18 Số 8 - Trang 1984-1999 - 2008
Peter M. Brown1, Cody L. Wienk2, Amy J. Symstad3
1Rocky Mountain Tree-Ring Research, 2901 Moore Lane, Ft. Collins, Colorado 80526 USA
2National Park Service, Midwest Regional Office, Omaha, Nebraska 68102 USA
3U.S. Geological Survey, Northern Prairie Wildlife Research Center, Hot Springs, South Dakota 57747 USA

Tóm tắt

Mount Rushmore National Memorial in the Black Hills of South Dakota is known worldwide for its massive sculpture of four of the United States' most respected presidents. The Memorial landscape also is covered by extensive ponderosa pine (Pinus ponderosa) forest that has not burned in over a century. We compiled dendroecological and forest structural data from 29 plots across the 517‐ha Memorial and used fire behavior modeling to reconstruct the historical fire regime and forest structure and compare them to current conditions. The historical fire regime is best characterized as one of low‐severity surface fires with occasional (>100 years) patches (<100 ha) of passive crown fire. We estimate that only ∼3.3% of the landscape burned as crown fire during 22 landscape fire years (recorded at ≥25% of plots) between 1529 and 1893. The last landscape fire was in 1893. Mean fire intervals before 1893 varied depending on spatial scale, from 34 years based on scar‐to‐scar intervals on individual trees to 16 years between landscape fire years. Modal fire intervals were 11–15 years and did not vary with scale. Fire rotation (the time to burn an area the size of the study area) was estimated to be 30 years for surface fire and 800+ years for crown fire. The current forest is denser and contains more small trees, fewer large trees, lower canopy base heights, and greater canopy bulk density than a reconstructed historical (1870) forest. Fire behavior modeling using the NEXUS program suggests that surface fires would have dominated fire behavior in the 1870 forest during both moderate and severe weather conditions, while crown fire would dominate in the current forest especially under severe weather. Changes in the fire regime and forest structure at Mount Rushmore parallel those seen in ponderosa pine forests from the southwestern United States. Shifts from historical to current forest structure and the increased likelihood of crown fire justify the need for forest restoration before a catastrophic wildfire occurs and adversely impacts the ecological and aesthetic setting of the Mount Rushmore sculpture.

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Ecological Applications

Tập 18 Số 8

1984-1999

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