Articles | Volume 12, issue 6
https://doi.org/10.5194/gmd-12-2401-2019
https://doi.org/10.5194/gmd-12-2401-2019
Model description paper
 | 
18 Jun 2019
Model description paper |  | 18 Jun 2019

Challenges in developing a global gradient-based groundwater model (G3M v1.0) for the integration into a global hydrological model

Robert Reinecke, Laura Foglia, Steffen Mehl, Tim Trautmann, Denise Cáceres, and Petra Döll

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Cited articles

Allen, P. M., Arnold, J. C., and Byars, B. W.: Downstream channel geometry for use in planning-level models, J. Am. Water Resour. As., 30, 663–671, https://doi.org/10.1111/j.1752-1688.1994.tb03321.x, 1994. 
Belcher, W. R. (Ed.): Death Valley Regional Ground-water Flow System, Nevada and California-Hydrogeologic Framework and Transient Ground-water Flow Model, U.S. Geological Survey Professional Paper, 408 pp., available at: https://pubs.usgs.gov/sir/2004/5205/ (last access: 1 June 2019), 2004. 
Belcher, W. R. and Sweetkind, D. S.: Death Valley regional groundwater flow system, Nevada and California – Hydrogeologic framework and transient groundwater flow model, U.S. Geological Survey Professional Paper 1711, 398 pp., available at: https://pubs.usgs.gov/pp/1711/ (last access: 1 June 2019), 2010. 
Costa, A. C., Foerster, S., de Araújo, J. C., and Bronstert, A.: Analysis of channel transmission losses in a dryland river reach in north-eastern Brazil using streamflow series, groundwater level series and multi-temporal satellite data, Hydrol. Process., 27, 1046–1060, https://doi.org/10.1002/hyp.9243, 2013. 
de Graaf, I. E. M., Sutanudjaja, E. H., van Beek, L. P. H., and Bierkens, M. F. P.: A high-resolution global-scale groundwater model, Hydrol. Earth Syst. Sci., 19, 823–837, https://doi.org/10.5194/hess-19-823-2015, 2015. 
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Short summary
G³M is a new global groundwater model (http://globalgroundwatermodel.org) that simulates lateral and vertical flows as well as exchanges with surface water bodies like rivers, lakes, and wetlands for the whole globe except Antarctica and Greenland. The newly developed model framework enables an efficient integration into established global hydrological models. This paper presents the G³M concept and specific model design decisions together with first results under a naturalized equilibrium.