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A geomorphic classification of ephemeral channels in a mountainous, arid region, southwestern Arizona, USA

机译:美国亚利桑那州西南部山区干旱地区短暂河道的地貌分类

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摘要

Despite the global abundance of arid-region ephemeral streams, hydrologic and geomorphic data for these systems are limited compared to their perennial counterparts. High spatial and temporal variability in flow makes hydrologic and geomorphic aspects of dryland ephemeral channels difficult to characterize. Perennial stream classifications have been extended to dryland ephemeral streams but do not adequately describe observed differences in channel geometry and characteristics of ephemeral channels in desert environments. We present a geomorphic classification for ephemeral streams in mountainous regions based on planform, degree of confinement, and composition of confining material. Five stream types were identified in the Sonoran desert of southwestern Arizona: (1) piedmont headwater, (2) bedrock, (3) bedrock with alluvium, (4) incised alluvium, and (5) braided channels. Nonparametric permutational multivariate analysis of variance for 101 surveyed reaches indicated differences (p < 0.001) in channel geometry and hydraulics among the five stream types. Nonmetric multidimensional scaling ordination identified the strongest channel geometry and hydraulic variables capable of distinguishing the five channel types, and a classification tree determined relative importance of these variables in the following order: width-to-depth ratio (W/D), stream gradient (S), stream power (Ω), and shear stress (τ). A classification tree and discriminant analysis used W/D, S, Ω, and τ for 86 study reaches on the U.S. Army Yuma Proving Ground (77% and 77% internal validation hit rate, respectively) to predict stream type of 15 separate study reaches on Barry Goldwater Air Force Range with 67% and 73% external validation hit rates, respectively. Differences in channel geometry among the five stream types reflect likely differences in hydrology, hydraulics, and sediment transport with implications for disturbance regime, channel adjustment to disturbance, and ecological sensitivity.
机译:尽管全球干旱地区的短暂河流数量众多,但与常年相比,这些系统的水文和地貌数据仍然有限。流量的高度时空变化使得旱地短暂河道的水文和地貌方面难以表征。多年生河流分类已扩展到旱地短暂河流,但没有充分描述沙漠环境中观测到的短暂河流通道几何形状和特征。我们提出了基于平面形式,限制程度和限制物质组成的山区短暂流的地貌分类。在亚利桑那州西南部的索诺兰沙漠中发现了五种水流类型:(1)山前源水,(2)基岩,(3)含冲积物的基岩,(4)切冲冲积物和(5)辫状河道。对101个被调查河段的方差的非参数排列多元分析表明,五种流类型在通道几何和水力方面存在差异(p <0.001)。非度量多维比例缩放排序确定了能够区分五种通道类型的最强通道几何形状和水力变量,分类树按以下顺序确定了这些变量的相对重要性:宽深比(W / D),流坡度( S),流功率(Ω)和剪切应力(τ)。分类树和判别分析使用W / D,S,Ω和τ对美国陆军尤马试验场上的86个研究范围(分别为77%和77%的内部验证命中率)进行预测,以预测15个单独研究范围的水流类型在Barry Goldwater Air Force Range上的外部验证命中率分别为67%和73%。五种水流类型之间的河道几何形状差异反映出水文,水力和泥沙输送的可能差异,这对扰动范围,对扰动的河道调整和生态敏感性具有影响。

著录项

  • 来源
    《Geomorphology 》 |2014年第15期| 164-175| 共12页
  • 作者单位

    Dept. of Geosciences, Colorado State University, Fort Collins, CO 80523-1482, USA;

    Dept. of Forest and Rangeland Stewardship, Colorado State University, Fort Collins, CO 80523-1472, USA, Graduate Degree Program in Ecology, Colorado State University, Fort Collins, CO 80523, USA;

    Dept. of Geosciences, Colorado State University, Fort Collins, CO 80523-1482, USA;

    Dept. of Forest and Rangeland Stewardship, Colorado State University, Fort Collins, CO 80523-1472, USA, Graduate Degree Program in Ecology, Colorado State University, Fort Collins, CO 80523, USA;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Stream classification; Desert stream; Ephemeral channel; Braided channel; Channel geometry; Arid region;

    机译:流分类;沙漠溪流;短暂通道;编织通道通道几何;干旱地区;

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