Stream Temperature Patterns over 35 Years in a Managed Forest of Western Washington

• Published in: Journal of the American Water Resources Association Vol. 51; no. 5; pp. 1418 - 1435
• Main Authors: Reiter, Maryanne, Bilby, Robert E., Beech, Storm, Heffner, John
• Format: Journal Article
• Language: English
• Published: Middleburg Blackwell Publishing Ltd 01.10.2015
• Subjects: Buffers; Channels; climate variability/change; Creeks & streams; Forest management; Forests; Marine; Northwest; stream temperature; Streams; timber harvest; Water quality; Water temperature; Watersheds; Washington DC; INE, USA, Washington; USA, Oregon, Deschutes R
• ISSN: 1093-474X; 1752-1688
• DOI: 10.1111/1752-1688.12324

Stream temperature changes as a result of forest practices have been a concern in the Pacific Northwest for several decades. As a result of this concern, stream protection requirements for forest lands were first adopted in the early 1970s and have become progressively more stringent. While there have been multiple studies examining the effects of stream protection buffers on water temperature, there are few studies examining temperature patterns over long periods on intensively managed forests. Water temperature in the upper Deschutes River watershed, Washington has been monitored since 1975 and represents one of the longest studies of water quality on managed forests in the Pacific Northwest. This data record, collected from basins of varying sizes, has enabled us to examine the combined effects of hydro‐climatic patterns and forest management on stream temperature. Effects of harvest conducted prior to buffer regulations were clearly identifiable and most pronounced on smaller streams. We were not able to detect any response on larger channels to more recent timber harvest where riparian buffers were required. This analysis also emphasizes that it is critical to account for changing climate when examining long‐term temperature patterns. We found that in many cases the temperature improvements associated with more stringent buffer requirements implemented over the last 35 years in the Deschutes watershed have been offset by warming climatic conditions.