Articles | Volume 23, issue 7
https://doi.org/10.5194/hess-23-2965-2019
https://doi.org/10.5194/hess-23-2965-2019
Research article
 | 
12 Jul 2019
Research article |  | 12 Jul 2019

Quantifying thermal refugia connectivity by combining temperature modeling, distributed temperature sensing, and thermal infrared imaging

Jessica R. Dzara, Bethany T. Neilson, and Sarah E. Null

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Cited articles

Bingham, Q. G., Neilson, B. T., Neale, C. M. U., and Cardenas, M. B.: Application of high-resolution, remotely sensed data for transient storage modeling parameter estimation, Water Resour. Res., 48, 1–15, https://doi.org/10.1029/2011WR011594, 2012. 
Bond, R. M., Stubblefield, A. P., and Kirk, R. W. Van: Sensitivity of summer stream temperatures to climate variability and riparian reforestation strategies, J. Hydrol. Reg. Stud. J. Hydrol., 4, 267–279, https://doi.org/10.1016/j.ejrh.2015.07.002, 2015. 
Brewitt, K. S. and Danner, E. M.: Spatio-temporal temperature variation influences juvenile steelhead (Oncorhynchus mykiss) use of thermal refuges, Ecosphere, 5, 1–26, 2014. 
Briggs, M. A., Lautz, L. K., McKenzie, J. M., Gordon, R. P., and Hare, D. K.: Using high-resolution distributed temperature sensing to quantify spatial and temporal variability in vertical hyporheic flux, Water Resour. Res., 48, 1–16, https://doi.org/10.1029/2011WR011227, 2012. 
Cardenas, M. B., Doering, M., Rivas, D. S., Galdeano, C., Neilson, B. T., and Robinson, C. T.: Analysis of the temperature dynamics of a proglacial river using time-lapse thermal imaging and energy balance modeling, J. Hydrol., 519, 1963–1973, https://doi.org/10.1016/j.jhydrol.2014.09.079, 2014. 
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In Nevada's Walker River, stream temperatures nearly always exceed optimal temperature thresholds for adult trout. We used high-resolution measured data to verify simulated stream temperatures and estimate the spatial distribution of cold-water pockets for fish. Irrigation return canals, beaver dams, and groundwater seeps were river features with cold-water, and the average distance between pockets of cold-water in this river was 2.8 km.
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