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. 2023 Feb 9;16(3):250–256. doi: 10.1038/s41561-023-01125-2

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© The Author(s) 2023

Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/.

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Fig. 3 — a,b, Spatial variations of the rooting-zone water-storage capacity, estimated by S_CWDX80 (a) and the apparent rooting depth z_CWDX80 (b). Values are remapped to 0.1° resolution. Blank grid cells (grey) are either permanent inland water bodies and ocean or locations with long-term accumulation of water deficits. Values are removed in grid cells where more than 99% is non-vegetation surface according to MODIS Landcover⁴².