Articles | Volume 28, issue 10
https://doi.org/10.5194/hess-28-2313-2024
https://doi.org/10.5194/hess-28-2313-2024
Research article
 | 
31 May 2024
Research article |  | 31 May 2024

Influence of irrigation on root zone storage capacity estimation

Fransje van Oorschot, Ruud J. van der Ent, Andrea Alessandri, and Markus Hrachowitz

Data sets

Dataset underlying Van Oorschot et al. (2024) Fransje van Oorschot https://doi.org/10.5281/zenodo.10869653

The Global Streamflow Indices and Metadata Archive - Part 1: Station catalog and Catchment boundary Hong Xuan Do et al. https://doi.org/10.1594/PANGAEA.887477

The Global Streamflow Indices and Metadata Archive (GSIM) - Part 2: Time Series Indices and Homogeneity Assessment Lukas Gudmundsson et al. https://doi.org/10.1594/PANGAEA.887470

CAMELS-AUS~v1: Hydrometeorological time series and landscape attributes for 222 catchments in Australia Keirnan Fowler et al. https://doi.org/10.1594/PANGAEA.921850

Hourly discharge database HydroCH Martina Kauzlaric et al. https://doi.org/10.5281/zenodo.7691294

ISIMIP2a atmospheric climate input data Stefan Lange and Matthias Büchner https://doi.org/10.48364/ISIMIP.886955

Historical Irrigation Dataset (HID) Stefan Siebert et al. https://doi.org/10.13019/M20599

Satellite-based Global Irrigation Water Use data set (2011-2018) Li Xin et al. https://doi.org/10.11888/Hydro.tpdc.271220

Present and future Köppen-Geiger climate classification maps at 1-km resolution H. E. Beck et al. https://doi.org/10.6084/m9.figshare.6396959

Model code and software

Scripts Van Oorschot et al. (2024) Fransje van Oorschot https://doi.org/10.5281/zenodo.11026863

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Short summary
Vegetation plays a crucial role in regulating the water cycle by transporting water from the subsurface to the atmosphere via roots; this transport depends on the extent of the root system. In this study, we quantified the effect of irrigation on roots at a global scale. Our results emphasize the importance of accounting for irrigation in estimating the vegetation root extent, which is essential to adequately represent the water cycle in hydrological and climate models.