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Geoscientific Model Development An interactive open-access journal of the European Geosciences Union
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Volume 11, issue 2
Geosci. Model Dev., 11, 521–540, 2018
https://doi.org/10.5194/gmd-11-521-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 3.0 License.
Geosci. Model Dev., 11, 521–540, 2018
https://doi.org/10.5194/gmd-11-521-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 3.0 License.

Model description paper 06 Feb 2018

Model description paper | 06 Feb 2018

An axisymmetric non-hydrostatic model for double-diffusive water systems

Koen Hilgersom et al.

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Cited articles

Arnon, A., Lensky, N. G., and Selker, J. S.: High-resolution temperature sensing in the Dead Sea using fiber optics, Water Resour. Res., 50, 1756–1772, https://doi.org/10.1002/2013WR014935, 2014.
Batchelor, G.: An introduction to fluid dynamics, Cambridge University Press, 615 pp., 1967.
Bennett, G., Reilly, T., and Hill, M.: Technical training notes in ground-water hydrology: radial flow to a well, Technical report, US Geological Survey; Books and Open-File Reports, 1990.
Bergman, T. L., Incropera, F. P., and Lavine, A. S.: Fundamentals of heat and mass transfer, John Wiley & Sons, 1048 pp., 2011.
Berthold, S. and Börner, F.: Detection of free vertical convection and double-diffusion in groundwater monitoring wells with geophysical borehole measurements, Environ. Geol., 54, 1547–1566, https://doi.org/10.1007/s00254-007-0936-y, 2008.
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This study models the local inflow of groundwater at the bottom of a stream with large density gradients between the groundwater and surface water. Modelling salt and heat transport in a water body is very challenging, as it requires large computation times. Due to the circular local groundwater inflow and a negligible stream discharge, we assume axisymmetry around the inflow, which is easily implemented in an existing model, largely reduces the computation times, and still performs accurately.
This study models the local inflow of groundwater at the bottom of a stream with large density...
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