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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. 2 — Stacked bars show the decomposing components of precipitation changes (ΔP) diagnosed from the atmospheric water vapor budget (Eq. (1)), including changes in evapotranspiration (ΔET), moisture advection (ΔQ_advt), moisture convergence (ΔQ_cnvg), and the residual term (Δε). Average changes across three cultivation maps for the eucalypt and switchgrass cultivation are aggregated for the entire global land area (left), the prescribed bioenergy crop cultivation regions (center) and the areas outside of the cultivation regions (right).