Comment on ‘Munz M, Krause S, Tecklenburg C, Binley A. Reducing monitoring gaps at the aquifer-river interface by modelling groundwater-surfacewater exchange flow patterns. Hydrological Processes. DOI: 10.1002/hyp.8080’-Reference-Cited by-同舟云学术

Comment on ‘Munz M, Krause S, Tecklenburg C, Binley A. Reducing monitoring gaps at the aquifer-river interface by modelling groundwater-surfacewater exchange flow patterns. Hydrological Processes. DOI: 10.1002/hyp.8080’

Published:2012-01-23 Issue:10 Volume:26 Page:1586-1588
ISSN:0885-6087
Container-title:Hydrological Processes
language:en
Short-container-title:Hydrol. Process.

Author:

Endreny T. A.¹,Lautz L. K.²

Affiliation:

1. Department of Environmental Resources Engineering; State University of New York College of Environmental Science and Forestry; 423 Baker Labs, 1 Forestry Dr.; Syracuse; NY; 13210; USA

2. 204 Heroy Geology Laboratory, Department of Earth Sciences; Syracuse University; Syracuse; NY; 13244; USA

Publisher

Wiley

Subject

Water Science and Technology

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1002/hyp.8410/fullpdf

Reference26 articles.

1. Patterns in Stream Longitudinal Profiles and Implications for Hyporheic Exchange Flow at the H.J. Andrews Experimental Forest, Oregon, USA;Anderson;Hydrological Processes,2005

2. Sinuosity-Driven Hyporheic Exchange in Meandering Rivers;Boano;Geophysical Research Letters,2006

3. Bedform-induced hyporheic exchange with unsteady flows;Boano;Advances in Water Resources,2007

4. Using high-resolution distributed temperature sensing to quantitatively describe spatial and temporal variability in vertical hyporheic flux;Briggs;Water Resources Research

5. A model for lateral hyporheic flow based on valley slope and channel sinuosity;Cardenas;Water Resources Research,2009

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3. A Comparison of Hyporheic Transport at a Cross-Vane Structure and Natural Riffle;Groundwater;2014-11-18

4. Effect of low-permeability layers on spatial patterns of hyporheic exchange and groundwater upwelling;Water Resources Research;2014-06

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