FIRE AND FOREST HISTORY AT MOUNT RUSHMORE

被引:81
作者
Brown, Peter M. [1 ]
Wienk, Cody L. [2 ]
Symstad, Amy J. [3 ]
机构
[1] Rocky Mt Tree Ring Res, Ft Collins, CO 80526 USA
[2] Midwest Reg Off, Natl Pk Serv, Omaha, NE 68102 USA
[3] US Geol Survey, No Prairie Wildlife Res Ctr, Hot Springs, SD 57747 USA
关键词
dendroecology; fire behavior; fire frequency; fire history; fire severity; forest structure; ponderosa pine; reference dynamics; restoration ecology;
D O I
10.1890/07-1337.1
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
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. re regime and forest structure and compare them to current conditions. The historical. re 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 similar to 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. re was in 1893. Mean. re 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. re years. Modal. re 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. re. 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. re 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 wild fire occurs and adversely impacts the ecological and aesthetic setting of the Mount Rushmore sculpture.
引用
收藏
页码:1984 / 1999
页数:16
相关论文
共 73 条
[1]  
AAGE JK, 1993, FIRE ECOLOGY PACIFIC
[2]  
Allen CD, 2002, ECOL APPL, V12, P1418
[3]  
ANDERSON HE, 1982, INT69 USDA FOR SERV
[4]  
[Anonymous], 2002, EXPLORING CUSTER 187
[5]   Fire, fuels and restoration of ponderosa pine-Douglas fir forests in the Rocky Mountains, USA [J].
Baker, William L. ;
Veblen, Thomas T. ;
Sherriff, Rosemary L. .
JOURNAL OF BIOGEOGRAPHY, 2007, 34 (02) :251-269
[6]  
Baker WL, 2001, CAN J FOREST RES, V31, P1205, DOI 10.1139/cjfr-31-7-1205
[7]  
Battaglia MA, 2007, THESIS COLORADO STAT
[8]   Decadal-scale dynamics at the Gus Pearson Natural Area: Evidence for inverse (a)symmetric competition? [J].
Biondi, F .
CANADIAN JOURNAL OF FOREST RESEARCH, 1996, 26 (08) :1397-1406
[9]  
BRADSHAW L, 1999, FIREFAMILY PLUS SOTW
[10]  
Brown J. K., 2000, RMRSGTR42 USDA FOR S, V2