Influences of vegetation disturbance on hydrogeomorphic response following wildfire

被引:11
|
作者
Hyde, Kevin D. [1 ,2 ]
Jencso, Kelsey [3 ]
Wilcox, Andrew C. [4 ]
Woods, Scott
机构
[1] Univ Montana, Coll Forestry & Conservat, Dept Ecosyst & Conservat Sci, Missoula, MT 59812 USA
[2] Univ Wyoming, Wyoming Ctr Environm Hydrol & Geophys, Laramie, WY 82071 USA
[3] Univ Montana, Dept Forest Management, Coll Forestry & Conservat, Missoula, MT 59812 USA
[4] Univ Montana, Dept Geosci, Missoula, MT 59812 USA
基金
美国国家科学基金会;
关键词
disturbance hydrology; overland flow; gully erosion; fire effects; vegetation disturbance; FIRE SEVERITY; BURN SEVERITY; PONDEROSA PINE; DEBRIS FLOWS; GULLY EROSION; MEDITERRANEAN ECOSYSTEM; HILLSLOPE EROSION; STATISTICAL-MODEL; SEDIMENT YIELDS; POSTFIRE RUNOFF;
D O I
10.1002/hyp.10691
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
Quantifying the linkages between vegetation disturbance by fire and the changes in hydrologic processes leading to post-fire erosional response remains a challenge. We measured the influence of fire severity, defined as vegetation disturbance (using a satellite-derived vegetation disturbance index, VDI), landscape features that organize hydrologic flow pathways (relief and elongation ratios), and pre-fire vegetation type on the probability of the occurrence of post-fire gully rejuvenation (GR). We combined field surveys across 270 burned low-order catchments (112 occurrences of GR) and geospatial analysis to generate a probabilistic model through logistic regression. VDI alone discriminated well between catchments where GR did and did not occur (area under the curve=0.78, model accuracy=0.72). The strong effect of vegetation disturbance on GR suggests that vegetation exerts a primary influence on the occurrence of infiltration excess run-off and post-fire erosion and that major gully erosion will not occur until fire consumes aboveground biomass. Other topographic and local factors also influenced GR response, including catchment elongation, per cent pre-fire shrub, mid-slope riparian vegetation, armoured headwaters, firehose effects, and concentration of severe burn in source areas. These factors highlight the need to consider vegetation effects in concert with local topography and site conditions to understand the propensity for flow accumulation leading to GR. We present a process-based conceptual hydrologic model where vegetation loss from fire decreases rainfall attenuation and surface roughness, leading to accelerated flow accumulation and erosion; these effects are also influenced by interactions between fire severity and landscape structure. The VDI metric provides a continuous measure of vegetation disturbance and, when placed in a hydrologic context, may improve quantitative analysis of burned-area susceptibility to erosive rainfall, hazard prediction, ecological effects of fire, landform evolution, and sensitivity to climate change. Copyright (c) 2015 John Wiley & Sons, Ltd.
引用
收藏
页码:1131 / 1148
页数:18
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