Uncertainties in vertical groundwater fluxes from 1-D steady state heat transport analyses caused by heterogeneity, multidimensional flow, and climate change-Reference-Cited by-同舟云学术

Uncertainties in vertical groundwater fluxes from 1-D steady state heat transport analyses caused by heterogeneity, multidimensional flow, and climate change

Published:2016-02 Issue:2 Volume:52 Page:813-826
ISSN:0043-1397
Container-title:Water Resources Research
language:en
Short-container-title:Water Resour. Res.

Author:

Irvine Dylan J.¹²,Cartwright Ian¹²,Post Vincent E.A.²³,Simmons Craig T.²³,Banks Eddie W.²³

Affiliation:

1. School of Earth, Atmosphere and Environment; Monash University; Clayton Victoria Australia

2. National Centre for Groundwater Research and Training; Adelaide South Australia Australia

3. School of the Environment; Flinders University; Adelaide South Australia Australia

Publisher

American Geophysical Union (AGU)

Subject

Water Science and Technology

Reference39 articles.

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3. A simple thermal mapping method for seasonal spatial patterns of groundwater-surface water interaction;Anibas;J. Hydrol.,2011

4. Temporal and spatial variations of shallow subsurface temperature as a record of lateral variations in groundwater flow;Bense;J. Geophys. Res.,2004

5. Rates of vertical groundwater movement estimated from the Earth's thermal profile;Bredehoeft;Water Resour. Res.,1965

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