| Environmental flow limits to global groundwater pumping IEM de Graaf, T Gleeson, LPH Van Beek, EH Sutanudjaja, MFP Bierkens Nature 574 (7776), 90-94, 2019 | 636 | 2019 |
| Global water resources and the role of groundwater in a resilient water future BR Scanlon, S Fakhreddine, A Rateb, I de Graaf, J Famiglietti, T Gleeson, ... Nature Reviews Earth & Environment 4 (2), 87-101, 2023 | 539 | 2023 |
| PCR-GLOBWB 2: a 5 arcmin global hydrological and water resources model EH Sutanudjaja, R Van Beek, N Wanders, Y Wada, JHC Bosmans, ... Geoscientific Model Development 11 (6), 2429-2453, 2018 | 435 | 2018 |
| A global-scale two-layer transient groundwater model: Development and application to groundwater depletion IEM de Graaf, RLPH van Beek, T Gleeson, N Moosdorf, O Schmitz, ... Advances in water Resources 102, 53-67, 2017 | 252 | 2017 |
| A high-resolution global-scale groundwater model IEM de Graaf, EH Sutanudjaja, LPH Van Beek, MFP Bierkens Hydrology and Earth System Sciences 19 (2), 823-837, 2015 | 230 | 2015 |
| High‐resolution modeling of human and climate impacts on global water resources Y Wada, IEM de Graaf, LPH van Beek Journal of Advances in Modeling Earth Systems 8 (2), 735-763, 2016 | 210 | 2016 |
| Dynamic attribution of global water demand to surface water and groundwater resources: Effects of abstractions and return flows on river discharges IEM De Graaf, LPH Van Beek, Y Wada, MFP Bierkens Advances in water resources 64, 21-33, 2014 | 158 | 2014 |
| PCR-GLOBWB 2: a 5 arcmin global hydrological and water resources model, Geosci. Model Dev., 11, 2429–2453 EH Sutanudjaja, R Van Beek, N Wanders, Y Wada, JHC Bosmans, ... | 136 | 2018 |
| Tradeoff of CO2 and CH4 emissions from global peatlands under water-table drawdown Y Huang, P Ciais, Y Luo, D Zhu, Y Wang, C Qiu, DS Goll, B Guenet, ... Nature Climate Change 11 (7), 618-622, 2021 | 127 | 2021 |
| Global distribution of groundwater‐vegetation spatial covariation S Koirala, M Jung, M Reichstein, IEM de Graaf, G Camps‐Valls, K Ichii, ... Geophysical Research Letters 44 (9), 4134-4142, 2017 | 115 | 2017 |
| Large‐scale assessment of delayed groundwater responses to drought J Hellwig, IEM De Graaf, M Weiler, K Stahl Water Resources Research 56 (2), e2019WR025441, 2020 | 104 | 2020 |
| GMD perspective: The quest to improve the evaluation of groundwater representation in continental-to global-scale models T Gleeson, T Wagener, P Döll, SC Zipper, C West, Y Wada, R Taylor, ... Geoscientific Model Development 14 (12), 7545-7571, 2021 | 82* | 2021 |
| A model comparison assessing the importance of lateral groundwater flows at the global scale IEM De Graaf, K Stahl Environmental Research Letters 17 (4), 044020, 2022 | 27 | 2022 |
| Hyper‐resolution continental‐scale 3‐D aquifer parameterization for groundwater modeling I de Graaf, L Condon, R Maxwell Water Resources Research 56 (5), e2019WR026004, 2020 | 20 | 2020 |
| Multicompartment depletion factors for water consumption on a global scale E Pierrat, M Dorber, I de Graaf, A Laurent, MZ Hauschild, M Rygaard, ... Environmental science & technology 57 (10), 4318-4331, 2023 | 16 | 2023 |
| A high resolution global scale groundwater model. IEM De Graaf, EH Sutanudjaja, LPH Van Beek, MFP Bierkens Hydrology & Earth System Sciences Discussions 11 (5), 2014 | 14 | 2014 |
| Cryosphere–groundwater connectivity is a missing link in the mountain water cycle M van Tiel, C Aubry-Wake, L Somers, C Andermann, F Avanzi, M Baraer, ... Nature Water 2 (7), 624-637, 2024 | 10 | 2024 |
| PCR-GLOBWB_model: PCR-GLOBWB version v2. 1.0 _beta_1 EH Sutanudjaja, R van Beek, N Wanders, Y Wada, J Bosmans, N Drost, ... Zenodo (https://doi. org/10.5281/zenodo. 247139), 2017 | 8 | 2017 |
| Limits to global groundwater consumption: Effects on groundwater levels and river low flows IEM de Graaf Utrecht University, 2016 | 8* | 2016 |
| PCR-GLOBWB 2: a 5 arcmin global hydrological and water resources model. Geosci. Model Dev. 2018; 11: 2429–2453. 10.5194 EH Sutanudjaja, R Van Beek, N Wanders, Y Wada, JHC Bosmans, ... gmd-11-2429-2018.[CrossRef][Academic Search], 0 | 8 | |
