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. 2023 Jul 11;14:4096. doi: 10.1038/s41467-023-39803-9

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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 Changes in precipitation (ΔP), evapotranspiration (ΔET), runoff (ΔRunoff), and water storage changes (ΔWSC) at the global scale for eucalypt (left) and switchgrass (right) cultivation scenarios averaged over the three cultivation maps. Changes in water balance components are also aggregated for different regions: b inside and outside of the cultivation region, c various humidity zones (i.e., arid, semiarid, subhumid and humid zones), and d wet and dry seasons in the monsoon regions. Note that ΔET and ΔRunoff are shown with reversed signs (−ΔET and −ΔRunoff) to be consistent with the ΔWSC deduced from the water balance (Eq. 5), and the directions of changes in these items are illustrated in the stylized legend.