Integrating regional and local monitoring data and assessment tools to evaluate habitat conditions and inform river restoration

Restoring degraded rivers requires initial assessment of the fluvial landscape to identify stressors and riverine features that can be enhanced. We associated local-scale river habitat data collected using standardized national monitoring tools with modeled regional water temperature and flow data o...

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Bibliographic Details
Main Authors: Andersen, T.K (Author), Berntsen, E.K (Author), Connor, J.M (Author), Kaufmann, P.R (Author), Mejia, F.H (Author), Torgersen, C.E (Author)
Format: Article
Language:English
Published: Elsevier B.V. 2021
Subjects:
Online Access:View Fulltext in Publisher
LEADER 03892nam a2200673Ia 4500
001 10.1016-j.ecolind.2021.108213
008 220427s2021 CNT 000 0 und d
020 |a 1470160X (ISSN) 
245 1 0 |a Integrating regional and local monitoring data and assessment tools to evaluate habitat conditions and inform river restoration 
260 0 |b Elsevier B.V.  |c 2021 
856 |z View Fulltext in Publisher  |u https://doi.org/10.1016/j.ecolind.2021.108213 
520 3 |a Restoring degraded rivers requires initial assessment of the fluvial landscape to identify stressors and riverine features that can be enhanced. We associated local-scale river habitat data collected using standardized national monitoring tools with modeled regional water temperature and flow data on mid-sized northwest U.S. rivers (30–60 m wide). We grouped these rivers according to quartiles of their modeled mean August water temperature and examined their physical habitat structure and flow. We then used principal components analysis to summarize the variation in several dimensions of physical habitat. We also compared local conditions in the Priest River, a river targeted for restoration of native salmonid habitat in northern Idaho, with those in other rivers of the region to infer potential drivers controlling water temperature. The warmest rivers had physical structure and fluvial characteristics typical of thermally degraded rivers, whereas the coldest rivers had higher mean summer flows and greater channel planform complexity. The Priest River sites had approximately twice as many deep residual pools (>50, >75, and >100 cm) and incision that averaged approximately twice that in the coldest rivers. Percentage fines and natural cover in the Priest were also more typical of the higher-temperature river groups. We found generally low instream cover and low levels of large wood both across the region and within the Priest River. Our approach enabled us to consider the local habitat conditions of a river in the context of other similarly sized rivers in the surrounding region. Understanding this context is important for identifying potential influences on river water temperature within the focal basin and for defining attainable goals for management and restoration of thermal and habitat conditions. © 2021 
650 0 4 |a accuracy assessment 
650 0 4 |a assessment method 
650 0 4 |a Ecosystems 
650 0 4 |a Environmental Monitoring and Assessment Program 
650 0 4 |a Environmental monitoring and assessment programs 
650 0 4 |a habitat structure 
650 0 4 |a Idaho 
650 0 4 |a Incision 
650 0 4 |a Incision 
650 0 4 |a Instream habitat 
650 0 4 |a In-stream habitats 
650 0 4 |a integrated approach 
650 0 4 |a landscape ecology 
650 0 4 |a Monitoring 
650 0 4 |a National river and stream assessment 
650 0 4 |a National Rivers and Streams Assessment 
650 0 4 |a Priest river 
650 0 4 |a Priest River 
650 0 4 |a Priest River 
650 0 4 |a Principal component analysis 
650 0 4 |a Restoration 
650 0 4 |a restoration ecology 
650 0 4 |a River assessments 
650 0 4 |a river channel 
650 0 4 |a river system 
650 0 4 |a river water 
650 0 4 |a Rivers 
650 0 4 |a Rivers and streams 
650 0 4 |a salmonid 
650 0 4 |a Salmonidae 
650 0 4 |a Salmonids 
650 0 4 |a Salmonids 
650 0 4 |a seasonal variation 
650 0 4 |a Stream assessment 
650 0 4 |a Stream flow 
650 0 4 |a Temperature 
650 0 4 |a United States 
650 0 4 |a water temperature 
650 0 4 |a Water temperature 
650 0 4 |a Water temperatures 
700 1 |a Andersen, T.K.  |e author 
700 1 |a Berntsen, E.K.  |e author 
700 1 |a Connor, J.M.  |e author 
700 1 |a Kaufmann, P.R.  |e author 
700 1 |a Mejia, F.H.  |e author 
700 1 |a Torgersen, C.E.  |e author 
773 |t Ecological Indicators