scholarly journals Improving representation of riparian vegetation shading in a regional stream temperature model using LiDAR data

2018 ◽  
Vol 624 ◽  
pp. 480-490 ◽  
Author(s):  
Pierre Loicq ◽  
Florentina Moatar ◽  
Yann Jullian ◽  
Stephen J. Dugdale ◽  
David M. Hannah
2019 ◽  
Vol 127 ◽  
pp. 125-134 ◽  
Author(s):  
Nicholas A. Giles ◽  
Meghna Babbar-Sebens ◽  
Raghavan Srinivasan ◽  
Darren L. Ficklin ◽  
Bradley Barnhart

2007 ◽  
Vol 200 (1-2) ◽  
pp. 217-224 ◽  
Author(s):  
Ching-Pin Tung ◽  
Yi-Chen E. Yang ◽  
Tsung-Yu Lee ◽  
Ming-Hsu Li

2019 ◽  
Vol 34 (2) ◽  
pp. 355-369 ◽  
Author(s):  
Luca Carraro ◽  
Marco Toffolon ◽  
Andrea Rinaldo ◽  
Enrico Bertuzzo

2019 ◽  
Vol 572 ◽  
pp. 308-328 ◽  
Author(s):  
Adam P. Piotrowski ◽  
Jaroslaw J. Napiorkowski

2014 ◽  
Vol 186 (11) ◽  
pp. 7489-7503 ◽  
Author(s):  
Ching-Pin Tung ◽  
Tsung-Yu Lee ◽  
Jr-Chuang Huang ◽  
Po-Wen Perng ◽  
Shih-Ji Kao ◽  
...  

2011 ◽  
Author(s):  
Christopher M. U. Neale ◽  
Hatim Geli ◽  
Saleh Taghvaeian ◽  
Ashish Masih ◽  
Robert T. Pack ◽  
...  

Land ◽  
2021 ◽  
Vol 10 (5) ◽  
pp. 519
Author(s):  
Nicole Durfee ◽  
Carlos G. Ochoa ◽  
Gerrad Jones

This study examined the relationship between stream temperature and environmental variables in a semiarid riparian corridor in northcentral Oregon, USA. The relationships between riparian vegetation cover, subsurface flow temperature, and stream temperature were characterized along an 800 m reach. Multiple stream temperature sensors were located along the reach, in open and closed canopy areas, with riparian vegetation cover ranging from 4% to 95%. A support vector regression (SVR) model was developed to assess the relationship between environmental characteristics and stream temperature at the larger valley scale. Results show that air temperature was highly correlated with stream temperature (Pearson’s r = 0.97). Based on the ANOVA, no significant (p < 0.05) differences in stream temperature levels were found among sensor locations at the valley scale, irrespective of percent vegetation cover. Channel subsurface temperature levels from an intermittent flow tributary were generally cooler than those in the perennial stream in the summer and warmer during winter months, indicating that the tributary may have a localized moderating effect on stream temperature. SVR model results showed that air temperature, followed by streamflow, was the strongest variable influencing stream temperature. In general, riparian area land cover showed little effect on stream temperature along the entire riparian corridor. This research indicates that air temperature, subsurface flow, and streamflow are important variables affecting the stream temperature variability observed in the study area.


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