Analysis of Alaskan burn severity patterns using remotely sensed data

Wildland fire is the dominant large-scale disturbance mechanism in the Alaskan boreal forest, and it strongly influences forest structure and function. In this research, patterns of burn severity in the Alaskan boreal forest are characterised using 24 fires. First, the relationship between burn severity and area burned is quantified using a linear regression. Second, the spatial correlation of burn severity as a function of topography is modelled using a variogram analysis. Finally, the relationship between vegetation type and spatial patterns of burn severity is quantified using linear models where variograms account for spatial correlation. These results show that: 1) average burn severity increases with the natural logarithm of the area of the wildfire, 2) burn severity is more variable in topographically complex landscapes than in flat landscapes, and 3) there is a significant relationship between burn severity and vegetation type in flat landscapes but not in topographically complex landscapes. These results strengthen the argument that differential flammability of vegetation exists in some boreal landscapes of Alaska. Additionally, these results suggest that through feedbacks between vegetation and burn severity, the distribution of forest vegetation through time is likely more stable in flat terrain than it is in areas with more complex topography.

[1]  R. D. Johnson,et al.  Using Landsat TM data to estimate carbon release from burned biomass in an Alaskan spruce forest complex , 2000 .

[2]  David L. Verbyla,et al.  Landscape-level interactions of prefire vegetation, burn severity, and postfire vegetation over a 16-year period in interior Alaska , 2005 .

[3]  E. Kasischke,et al.  Stand-level effects of soil burn severity on postfire regeneration in a recently burned black spruce forest , 2005 .

[4]  S. Payette,et al.  A Systems Analysis of the Global Boreal Forest: Fire as a controlling process in the North American boreal forest , 1992 .

[5]  Leslie A. Viereck,et al.  Decadal observations of tree regeneration following fire in boreal forests , 2004 .

[6]  Herman H. Shugart,et al.  A Systems Analysis of the Global Boreal Forest , 1993 .

[7]  A. McGuire,et al.  Global climate change and terrestrial net primary production , 1993, Nature.

[8]  D. Verbyla,et al.  Evaluation of remotely sensed indices for assessing burn severity in interior Alaska using Landsat TM and ETM , 2005 .

[9]  Z. Chrosciewicz,et al.  Evaluation of Fire-produced Seedbeds for Jack Pine Regeneration in Central Ontario , 1974 .

[10]  John E. Walsh,et al.  IMPACTS OF LARGE‐SCALE ATMOSPHERIC–OCEAN VARIABILITY ON ALASKAN FIRE SEASON SEVERITY , 2005 .

[11]  Lucinda B. Johnson,et al.  Analyzing spatial and temporal phenomena using geographical information systems , 1990, Landscape Ecology.

[12]  E. Kasischke,et al.  Analysis of the patterns of large fires in the boreal forest region of Alaska , 2002 .

[13]  O. Zackrisson,et al.  Influence of forest fires on the North Swedish boreal forest , 1977 .

[14]  J. Yarie,et al.  Forest fire cycles and life tables: a case study from interior Alaska , 1981 .

[15]  N. Benson,et al.  Landscape Assessment: Ground measure of severity, the Composite Burn Index; and Remote sensing of severity, the Normalized Burn Ratio , 2006 .

[16]  R A Johnson,et al.  Two-sample rank tests for detecting changes that occur in a small proportion of the treated population. , 1987, Biometrics.

[17]  Gordon K. Smyth,et al.  A Conditional Likelihood Approach to Residual Maximum Likelihood Estimation in Generalized Linear Models , 1996 .

[18]  E. Johnson,et al.  Process and patterns of duff consumption in the mixedwood boreal forest , 2002 .

[19]  J. W. Wagtendonk,et al.  Comparison of AVIRIS and Landsat ETM+ detection capabilities for burn severity , 2004 .

[20]  C. T. Dyrness,et al.  The effects of experimental fires on black spruce forest floors in interior Alaska , 1983 .

[21]  Edward A. Johnson,et al.  Wildfires in the southern Canadian Rocky Mountains and their relationship to mid-tropospheric anomalies , 1993 .

[22]  D. Mann,et al.  Vegetation and soil development at an upland taiga site, Alaska , 1999 .

[23]  D. Foster Vegetation development following fire in Picea mariana (black spruce). Pleurozium forests of south-eastern Labrador, Canada , 1985 .

[24]  P. Richard,et al.  Effects of fire severity and initial tree composition on understorey vegetation dynamics in a boreal landscape inferred from chronosequence and paleoecological data , 2005 .

[25]  E. Johnson,et al.  Geomorphic principles of terrain organization and vegetation gradients , 2000 .

[26]  R. A. Norum,et al.  Artificial regeneration of trees and tall shrubs in experimentally burned upland black spruce/feather moss stands in Alaska , 1983 .

[27]  D. Greene,et al.  Recruitment of Picea mariana, Pinus banksiana, and Populus tremuloides across a burn severity gradient following wildfire in the southern boreal forest of Quebec , 2004 .

[28]  E. Johnson,et al.  The Relative Importance of Fuels and Weather on Fire Behavior in Subalpine Forests , 1995 .