Flood Effects on an Alaskan Stream Restoration Project: The Value of Long-Term Monitoring super(1)

• Published in: Journal of the American Water Resources Association Vol. 45; no. 6; pp. 1424 - 1433
• Main Authors: Densmore, Roseann V, Karle, Kenneth F
• Format: Journal Article
• Language: English
• Published: 01.12.2009
• Subjects: Channels; Floods; Monitoring; Restoration; Sediments; Streams; Vegetation; Water resources; USA, Alaska, Denali Natl. Park; INE, USA, Alaska; IN, North Pacific, Alaskan Stream
• ISSN: 1093-474X; 1752-1688
• DOI: 10.1111/j.1752-1688.2009.00373.x

Densmore, Roseann V. and Kenneth F. Karle, 2009. Flood Effects on an Alaskan Stream Restoration Project: The Value of Long-Term Monitoring. Journal of the American Water Resources Association (JAWRA) 45(6):1424-1433. Abstract: On a nationwide basis, few stream restoration projects have long-term programs in place to monitor the effects of floods on channel and floodplain configuration and floodplain vegetation, but long-term and event-based monitoring is required to measure the effects of these stochastic events and to use the knowledge for adaptive management and the design of future projects. This paper describes a long-term monitoring effort (15years) on a stream restoration project in Glen Creek in Denali National Park and Preserve in Alaska. The stream channel and floodplain of Glen Creek had been severely degraded over a period of 80years by placer mining for gold, which left many reaches with unstable and incised streambeds without functioning vegetated floodplains. The objectives of the original project, initiated in 1991, were to develop and test methods for the hydraulic design of channel and floodplain morphology and for floodplain stabilization and riparian habitat recovery, and to conduct research and monitoring to provide information for future projects in similar degraded watersheds. Monitoring methods included surveyed stream cross-sections, vegetation plots, and aerial, ground, and satellite photos. In this paper we address the immediate and outlying effects of a 25-year flood on the stream and floodplain geometry and riparian vegetation. The long-term monitoring revealed that significant channel widening occurred following the flood, likely caused by excessive upstream sediment loading and the fairly slow development of floodplain vegetation in this climate. Our results illustrated design flaws, particularly in regard to identification and analysis of sediment sources and the dominant processes of channel adjustment.