Articles | Volume 22, issue 12
https://doi.org/10.5194/hess-22-6163-2018
https://doi.org/10.5194/hess-22-6163-2018
Review article
 | 
30 Nov 2018
Review article |  | 30 Nov 2018

Toward a conceptual framework of hyporheic exchange across spatial scales

Chiara Magliozzi, Robert C. Grabowski, Aaron I. Packman, and Stefan Krause

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Cited articles

Abbe, T. B. and Montgomery, D. R.: Patterns and processes of wood debris accumulation in the Queets river basin, Washington, Geomorphology, 51, 81–107, 2003. a
Allen, D. J., Darling, W. G., Gooddy, D. C., Lapworth, D. J., Newell, A. J., Williams, A. T., Allen, D., and Abesser, C.: Interaction between groundwater, the hyporheic zone and a Chalk stream: a case study from the River Lambourn, UK, Hydrogeol. J., 18, 1125–1141, 2010. a
Anderson, J. K., Wondzell, S. M., Gooseff, M. N., and Haggerty, R.: Patterns in stream longitudinal profiles and implications for hyporheic exchange flow at the H.J. Andrews Experimental Forest, Oregon, USA, Hydrol. Proc., 19, 2931–2949, 2005. a, b, c, d
Angermann, L., Krause, S., and Lewandowski, J.: Application of heat pulse injections for investigating shallow hyporheic flow in a lowland river, Water Resour. Res., 48, W00P02, https://doi.org/10.1029/2012WR012564, 2012. a, b, c, d, e, f, g
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Short summary
The hyporheic zone is the area below riverbeds where surfacewater and groundwater mix. Hyporheic flow is linked to river processes and functions, but research to date has not sufficiently addressed how factors operating at different scales in time and space drive hyporheic flow variations at reach and larger scales. This review presents the scale-specific processes and interactions that control hyporheic flow, and a case study showing how valley factors affect its expression at the reach scale.