Brown Peter M, Wienk Cody L, Symstad Amy J
Rocky Mountain Tree-Ring Research, 2901 Moore Lane, Ft. Collins, Colorado 80526, USA.
Ecol Appl. 2008 Dec;18(8):1984-99. doi: 10.1890/07-1337.1.
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 approximately 3.3% of the landscape burned as crown fire during 22 landscape fire years (recorded at > or = 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.
南达科他州黑山地区的拉什莫尔山国家纪念公园以其雕刻的四位美国最受尊敬总统的巨型雕塑而闻名于世。纪念公园的景观还覆盖着大面积的黄松(Pinus ponderosa)森林,这片森林已经有一个多世纪没有发生过火灾了。我们收集了这片517公顷纪念公园内29个样地的树木年代生态学和森林结构数据,并利用火灾行为模型重建历史火灾状况和森林结构,并将其与当前状况进行比较。历史火灾状况的最佳特征是低强度地表火,偶尔(>100年)出现小块(<100公顷)被动树冠火。我们估计,在1529年至1893年的22个景观火灾年份(记录在≥25%的样地)中,只有约3.3%的景观发生了树冠火。上一次景观火灾发生在1893年。1893年之前的平均火灾间隔因空间尺度而异,从基于单棵树木疤痕到疤痕间隔的34年到景观火灾年份之间的16年不等。典型火灾间隔为11 - 15年,且不随尺度变化。地表火的火灾轮替(燃烧研究区域大小面积所需的时间)估计为30年,树冠火则超过800年。与重建的历史(1870年)森林相比,当前的森林更茂密,小树更多,大树更少,树冠基部高度更低,树冠体积密度更大。使用NEXUS程序进行的火灾行为模型表明,在1870年的森林中,无论是在中等还是恶劣天气条件下,地表火都将主导火灾行为,而在当前森林中,树冠火将占主导地位,尤其是在恶劣天气下。拉什莫尔山火灾状况和森林结构的变化与美国西南部黄松森林的情况相似。从历史森林结构向当前森林结构的转变以及树冠火发生可能性的增加,证明了在灾难性野火发生并对拉什莫尔山雕塑的生态和美学环境产生不利影响之前进行森林恢复的必要性。