2022
DOI: 10.1038/s43017-022-00287-8
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A planetary boundary for green water

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Cited by 163 publications
(150 citation statements)
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“…In comparing historical and pre-industrial states of the freshwater cycle, we followed the general approach of Wang-Erlandsson et al (20) with certain changes related to data and methodology. First, instead of custom runs using the global dynamic vegetation model LPJmL 5.1 forced with bias-corrected and downscaled CMIP6 climate data (20), we used the ISIMIP 2b global hydrological model outputs that are forced with bias-corrected climate data from CMIP5 (39). Second, we chose to define the grid cell scale local pre-industrial bounds strictly cell-wise and performed annual aggregation by monthly averaging.…”
Section: Methodsmentioning
confidence: 99%
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“…In comparing historical and pre-industrial states of the freshwater cycle, we followed the general approach of Wang-Erlandsson et al (20) with certain changes related to data and methodology. First, instead of custom runs using the global dynamic vegetation model LPJmL 5.1 forced with bias-corrected and downscaled CMIP6 climate data (20), we used the ISIMIP 2b global hydrological model outputs that are forced with bias-corrected climate data from CMIP5 (39). Second, we chose to define the grid cell scale local pre-industrial bounds strictly cell-wise and performed annual aggregation by monthly averaging.…”
Section: Methodsmentioning
confidence: 99%
“…To acknowledge these limitations, recent studies have proposed sub-dividing the freshwater PB into blue and green water components and adopting a bottom-up, area-based approach (1,11,20). Recently, a provisional analysis of Wang-Erlandsson et al (20) proposed that the freshwater PB should describe change rather than use, and found a likely transgression of the green water component. Yet, previous works have not assessed how the blue and green water components coevolve, or where the geographical hotspots of change are located.…”
Section: Main Textmentioning
confidence: 99%
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