H23H-1669
Spatial and Temporal Stream Temperature Response to Contemporary Forest Harvesting in the Oregon Coast Range

Tuesday, 15 December 2015
Poster Hall (Moscone South)
Kevin D. Bladon, Oregon State University, Forest Engineering, Resources, and Management, Corvallis, OR, United States, Jeffrey T. Light, Plum Creek Timber Company, Toledo, OR, United States and Mark Teply, Cramer Fish Sciences, Lacey, WA, United States
Abstract:
Historical research at the Alsea Watershed Study (1958-1973), in the Oregon Coast Range, demonstrated that clear-cut harvesting, with complete removal of riparian vegetation, can result in large and dramatic changes in mean daily, maximum daily, diurnal variation, and annual patterns in stream temperature (Ts). This previous research was instrumental in the addition of regulations in the Oregon Forest Practices Act of 1971, necessitating retention of streamside vegetation (riparian management zones) in harvest units to maintain water quality and aquatic habitat. Due to the ecological importance of Ts, preventing or mitigating changes in the thermal regime following land use activities, such as forest harvesting, is a primary focus of contemporary forest watershed management. The Alsea Watershed Study Revisited (2006-Present) has provided a unique opportunity to investigate the Ts responses to contemporary forest harvesting practices and compare these with the impacts from the 1960’s harvest. In general, Ts increases from late spring through about mid-July, with peak Ts occuring between about mid-July and mid-August, after which Ts decreases into the fall. During the pre-harvest period (2006-2008; n=244) the June to September mean daily maximum Ts was 13.0°C in Flynn Creek (control) and 12.0°C in Needle Branch (harvested). In the post-harvest period (2010-2012; n=240) the June to September mean daily maximum Ts was 12.4°C in Flynn Creek (control) and 12.0°C in Needle Branch (harvested). Similarly, the difference (Flynn Ck – Needle Branch) in 7 day moving mean of daily maximum Ts decreased from the pre-harvest (1.0°C) to the post-harvest (0.3°C) period, which was principally driven by a decrease in Ts in the control catchment. Longitudinal sampling of Ts within Needle Branch indicated a cooling trend such that the slight increases in post-harvest Ts weren’t detectable in downstream, unharvested stream reaches.