4.6 Article Proceedings Paper

Post-disturbance sediment recovery: Implications for watershed resilience

Journal

GEOMORPHOLOGY
Volume 305, Issue -, Pages 61-75

Publisher

ELSEVIER SCIENCE BV
DOI: 10.1016/j.geomorph.2017.08.039

Keywords

Sediment recovery; Disturbance; Resilience; Post-disturbance recovery

Funding

  1. National Fire Plan
  2. National Science Foundation RAPID Award [EAR1410472]
  3. Gladys Cole Memorial Fund (Quaternary Geology and Geomorphology Division, Geological Society of America)
  4. National Park Service and Rocky Mountain National Park

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Sediment recovery following disturbances is a measure of the time required to attain pre-disturbance sediment fluxes. Insight into the controls on recovery processes and pathways builds understanding of geomorphic resilience. We assess post-disturbance sediment recovery in three small (1.5-100 km(2)), largely unaltered watersheds within the northern Colorado Rocky Mountains affected by wildfires, floods, and debris flows. Disturbance regimes span 10(2) (floods, debris flows) to 10(3) years (wildfires). For all case studies, event sediment recovery followed a nonlinear pattern: initial high sediment flux during single precipitation events or high annual snow melt runoff followed by decreasing sediment fluxes over time. Disturbance interactions were evaluated after a high-severity fire within the South Fork Cache la Poudre basin was followed by an extreme flood one year post-fire. This compound disturbance hastened suspended sediment recovery to pre-fire concentrations 3 years after the fire. Wildfires over the last 1900 YBP in the South Fork basin indicate fire recurrence intervals of similar to 600 years. Debris flows within the upper Colorado River basin over the last two centuries have shifted the baseline of sediment recovery caused by anthropogenic activities that increased debris flow frequency. An extreme flood on North St. Vrain Creek with an impounding reservoir resulted in extreme sedimentation that led to a physical state change. We introduce an index of resilience as sediment recovery/disturbance recurrence interval, providing a relative comparison between sites. Sediment recovery and channel form resilience may be inversely related because of high or low physical complexity in streams. We propose management guidelines to enhance geomorphic resilience by promoting natural processes that maintain physical complexity. Finally, sediment connectivity within watersheds is an additional factor to consider when establishing restoration treatment priorities. (C) 2017 Elsevier B.V. All rights reserved.

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