Geomorphic characteristics influencing post-fire river response in mountain streams

IF 3.1 2区 地球科学 Q2 GEOGRAPHY, PHYSICAL Geomorphology Pub Date : 2024-10-03 DOI:10.1016/j.geomorph.2024.109446
Shayla Triantafillou, Ellen Wohl
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Abstract

As wildfires increase in frequency and severity, there is a growing interest in understanding river response to the wildfire disturbance cascade. Numerous headwater mountain catchments within the Cache la Poudre (Poudre) River basin in the Colorado Front Range, USA burned severely and extensively during the 2020 Cameron Peak fire. Debris flows and flash floods occurred in many of these catchments triggered by convective storms after the fire. The downstream effects of the floods and sediment varied along a continuum from attenuated and largely contained within the catchment, to releasing substantial volumes of water and sediment to the Poudre River. We conceptualize these catchments as exhibiting decreasing absorbance of post-fire disturbance along the continuum described above based on the geomorphic evidence of relative sediment export. We conceptualize characteristics on different spatial scales as driving or resisting response to disturbance and therefore impacting the absorbing capacity (ability to attenuate post-fire fluxes) of the catchment. As the magnitude of resisting characteristics increases at the catchment, inter- and intra- reach scales, we hypothesize that a catchment will increasingly absorb the impacts of the wildfire disturbance cascade. We conducted longitudinally continuous surveys to measure reach-scale characteristics within each study catchment. We focus on the catchment- and reach-scale geomorphic, vegetation, and burn characteristics. The floods observed at the study catchments illustrate fire influencing the elevation above which rainfall-induced flooding occurs due to the efficient conveyance of water from hillslopes to channels after wildfire. Results suggest that inter- and intra-reach spatial heterogeneity are better aligned with absorbance capacity than catchment-scale characteristics: greater absorbing capacity is associated with greater longitudinal variations in floodplain/channel width and more reaches with wide floodplains, low channel gradients, beaver-modified topography, and multi-stem deciduous vegetation. We connect the capacity to absorb the impacts of disturbance as informing the catchment response to wildfire disturbance.
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影响山涧河流火灾后反应的地貌特征
随着野火发生的频率和严重程度的增加,人们越来越有兴趣了解河流对野火扰动级联的反应。在 2020 年的卡梅伦峰大火中,美国科罗拉多前沿山脉的卡奇拉普德雷河(普德雷河)流域内的许多上游山区集水区被大面积严重烧毁。火灾发生后,对流风暴引发了许多流域的泥石流和山洪。洪水和沉积物对下游的影响各不相同,有的会减弱并基本控制在集水区内,有的则会将大量的水和沉积物释放到 Poudre 河中。根据相对沉积物输出的地貌证据,我们认为这些集水区对火灾后扰动的吸收能力在上述连续过程中呈递减趋势。我们将不同空间尺度上的特征概念化为对扰动的驱动或抵制响应,从而影响集水区的吸收能力(衰减火灾后流量的能力)。随着集水区、集水区间和集水区内抵御特征的增加,我们假设集水区将越来越多地吸收野火干扰级联的影响。我们进行了纵向连续调查,以测量每个研究流域内的流域尺度特征。我们重点研究了集水区和流域尺度的地貌、植被和燃烧特征。在研究集水区观察到的洪水表明,由于野火后山坡上的水被有效地输送到渠道,火灾影响了降雨引起的洪水发生的海拔高度。研究结果表明,与流域尺度特征相比,流域间和流域内的空间异质性更符合吸水能力:更大的吸水能力与更大的洪泛区/河道宽度纵向变化以及更多具有宽洪泛区、低河道坡度、海狸改良地形和多茎落叶植被的流域有关。我们将吸收干扰影响的能力与集水区对野火干扰的反应联系起来。
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来源期刊
Geomorphology
Geomorphology 地学-地球科学综合
CiteScore
8.00
自引率
10.30%
发文量
309
审稿时长
3.4 months
期刊介绍: Our journal''s scope includes geomorphic themes of: tectonics and regional structure; glacial processes and landforms; fluvial sequences, Quaternary environmental change and dating; fluvial processes and landforms; mass movement, slopes and periglacial processes; hillslopes and soil erosion; weathering, karst and soils; aeolian processes and landforms, coastal dunes and arid environments; coastal and marine processes, estuaries and lakes; modelling, theoretical and quantitative geomorphology; DEM, GIS and remote sensing methods and applications; hazards, applied and planetary geomorphology; and volcanics.
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