What should these rivers look like? Historical range of variability and human impacts in the Colorado Front Range, USA

被引:50
|
作者
Wohl, Ellen [1 ]
机构
[1] Colorado State Univ, Dept Geosci, Ft Collins, CO 80523 USA
关键词
Colorado; historical range of variability; mountain rivers; instream wood; LARGE WOODY DEBRIS; CHANNEL MORPHOLOGY; SEDIMENT DYNAMICS; MOUNTAIN STREAMS; FOREST STREAMS; ORGANIC DEBRIS; PATTERNS; DAMS;
D O I
10.1002/esp.2180
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
Historical range of variability (HRV) describes the range of temporal and spatial variations in river variables such as flow regime or channel planform prior to intensive human alteration of the ecosystem. In mountainous river networks, HRV is most usefully applied to spatially differentiated geomorphic process domains with distinctive form and process. Using the Colorado Front Range as an example, three examples of how knowledge of HRV can assist river management and restoration are discussed. The examples involve instream wood load and channel morphology, beaver colonies and valley-bottom form and process, and flow thresholds in regulated rivers. The question of what a river should look like - that is, what range of process and form the river included prior to intensive human alteration - can be addressed by (i) placing the river within a process domain, (ii) establishing correlations between form parameters that can be remotely sensed and reach-scale process and form, so that the spatial extent, connectivity, and rarity of process domains within a river network or a region can be quickly assessed, (iii) inferring characteristics of the river prior to intensive alteration by documenting characteristics of the least altered reference rivers and by using proxy indicators of pre-alteration conditions, and (iv) establishing process thresholds that must be exceeded to maintain form (e. g. flow thresholds to mobilize bed sediment). Once this context has been established, resource managers can better evaluate the options for restoring altered riverine form and function. Copyright (C) 2011 John Wiley & Sons, Ltd.
引用
收藏
页码:1378 / 1390
页数:13
相关论文
共 50 条
  • [31] Historical range of variability in eastern Cascades forests, Washington, USA
    James K. Agee
    [J]. Landscape Ecology, 2003, 18 : 725 - 740
  • [32] Historical, Observed, and Modeled Wildfire Severity in Montane Forests of the Colorado Front Range
    Sherriff, Rosemary L.
    Platt, Rutherford V.
    Veblen, Thomas T.
    Schoennagel, Tania L.
    Gartner, Meredith H.
    [J]. PLOS ONE, 2014, 9 (09):
  • [33] SPATIAL VARIABILITY OF CARBONYL COMPOUND CONCENTRATIONS MEASURED ALONG THE COLORADO FRONT RANGE
    ANDERSON, LG
    LANNING, JA
    PROUTY, E
    EISENHARDT, R
    PRIBIL, M
    [J]. ABSTRACTS OF PAPERS OF THE AMERICAN CHEMICAL SOCIETY, 1995, 209 : 48 - ENVR
  • [36] Ecological response of step-pool streams to wildfire in the Front Range of Colorado (USA)
    O’Dowd, Alison P.
    Solverson, Anna P.
    Chin, Anne
    [J]. Special Paper of the Geological Society of America, 2024, 562 : 80 - 94
  • [37] CONTROLS ON THE LONGITUDINAL DISTRIBUTION OF CHANNEL-SPANNING LOGJAMS IN THE COLORADO FRONT RANGE, USA
    Wohl, E.
    Beckman, N.
    [J]. RIVER RESEARCH AND APPLICATIONS, 2014, 30 (01) : 112 - 131
  • [38] Factors determining alpine species distribution on Goliath Peak, Front Range, Colorado, USA
    Boyce, RL
    Clark, R
    Dawson, C
    [J]. ARCTIC ANTARCTIC AND ALPINE RESEARCH, 2005, 37 (01) : 88 - 96
  • [39] From on high: Geochemistry of alpine springs, Niwot Ridge, Colorado Front Range, USA
    Fields, Jordan F.
    Dethier, David P.
    [J]. HYDROLOGICAL PROCESSES, 2019, 33 (12) : 1756 - 1774
  • [40] Internal Structure of the Green Lake 5 Rock Glacier, Colorado Front Range, USA
    Leopold, M.
    Williams, M. W.
    Caine, N.
    Voelkel, J.
    Dethier, D.
    [J]. PERMAFROST AND PERIGLACIAL PROCESSES, 2011, 22 (02) : 107 - 119