Abstract
Rainfall events are globally becoming less frequent but more intense under a changing climate, thereby shifting climatic conditions for terrestrial vegetation independent of annual rainfall totals1,2,3. However, it remains uncertain how changes in daily rainfall variability are affecting global vegetation photosynthesis and growth3,4,5,6,7,8,9,10,11,12,13,14,15,16,17. Here we use several satellite-based vegetation indices and field observations indicative of photosynthesis and growth, and find that global annual-scale vegetation indices are sensitive to the daily frequency and intensity of rainfall, independent of the total amount of rainfall per year. Specifically, we find that satellite-based vegetation indices are sensitive to daily rainfall variability across 42 per cent of the vegetated land surfaces. On average, the sensitivity of vegetation to daily rainfall variability is almost as large (95 per cent) as the sensitivity of vegetation to annual rainfall totals. Moreover, we find that wet-day frequency and intensity are projected to change with similar magnitudes and spatial extents as annual rainfall changes. Overall, our findings suggest that daily rainfall variability and its trends are affecting global vegetation photosynthesis, with potential implications for the carbon cycle and food security.
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Data availability
The data used and created in the study are available in two repositories. The processed data inputs are available on Zenodo at https://doi.org/10.5281/zenodo.10947071 (ref. 97). The output data and reduced-size example input data are available on Zenodo at https://doi.org/10.5281/zenodo.13551521 (ref. 98). All datasets used in the study are freely available and were obtained as follows. The MODIS NDVI product can be obtained from https://modis.gsfc.nasa.gov/data/dataprod/mod13.php. AVHRR NDVI can be obtained from https://www.ncei.noaa.gov/data/land-normalized-difference-vegetation-index/access/. GOME-2 SIF can be downloaded from https://daac.ornl.gov/SIF-ESDR/guides/MetOpA_GOME2_SIF.html. OCO-2 SIF can be obtained from https://disc.gsfc.nasa.gov/datasets/OCO2_L2_Lite_SIF_10r/summary. The MT-DCA vegetation optical depth dataset retrieved from SMAP is freely available at https://doi.org/10.5281/zenodo.5579549. AIRS humidity and air temperature data are available at https://airs.jpl.nasa.gov/data/get-data/standard-data/. The MODIS land surface temperature product can obtained from https://lpdaac.usgs.gov/products/myd11c2v006/. MERRA-2 precipitation data can be accessed at https://gmao.gsfc.nasa.gov/reanalysis/MERRA-2/data_access/. CERES radiation can be accessed at https://asdc.larc.nasa.gov/project/CERES/CER_SYN1deg-Day_Terra-Aqua-MODIS_Edition4A. SMAP soil moisture can be obtained from https://nsidc.org/data/smap/data. GPM precipitation outputs are available at https://gpm.nasa.gov/data/directory. CPC precipitation data are available at https://psl.noaa.gov/data/gridded/data.cpc.globalprecip.html. REGEN precipitation data are available at https://thredds-x.ipsl.fr/thredds/catalog/FROGs/REGEN_ALL_V1-2019/catalog.html. FLUXNET gross primary production observations can be obtained from https://fluxnet.org. CMIP6 rainfall projections can be obtained from https://cds.climate.copernicus.eu.
Code availability
The code is available on Zenodo at https://doi.org/10.5281/zenodo.13551521 (ref. 98) to both create the figures and conduct the analysis. This repository includes the main analysis outputs and example input data. The full processed data inputs are available on Zenodo at https://doi.org/10.5281/zenodo.10947071 (ref. 97).
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Acknowledgements
A.F.F. was supported by an appointment to the NASA Postdoctoral Program at the NASA Goddard Space Flight Center, administered by Oak Ridge Associated Universities under contract with NASA. A.F.F. was also partly supported by a NASA Terrestrial Ecology Program scoping study for dryland ecosystems. A.G.K. was supported by the Alfred P. Sloan Foundation and by NSF DEB 1942133. W.K.S. and B.P. acknowledge support from the NASA Carbon Cycle Science grant number 80NSSC23K0109. M.A. acknowledges Swiss National Science Foundation grant number 206603. L.W. acknowledges partial support from the US National Science Foundation (DEB-2307257 and DEB-2406931). USDA is an equal-opportunity employer and provider. We acknowledge the World Climate Research Programme, which, through its Working Group on Coupled Modelling, coordinated and promoted CMIP6. We thank the climate modelling groups for producing and making available their model output, the Earth System Grid Federation (ESGF) for archiving the data and providing access, and the multiple funding agencies that support CMIP6 and ESGF. This work used eddy covariance data acquired and shared by the FLUXNET community, including these networks: AmeriFlux, AfriFlux, AsiaFlux, CarboAfrica, CarboEuropeIP, CarboItaly, CarboMont, ChinaFlux, Fluxnet-Canada, GreenGrass, ICOS, KoFlux, LBA, NECC, OzFlux-TERN, TCOS-Siberia and USCCC. The FLUXNET eddy covariance data processing and harmonization was carried out by the ICOS Ecosystem Thematic Center, AmeriFlux Management Project and Fluxdata project of FLUXNET, with the support of CDIAC, and the OzFlux, ChinaFlux and AsiaFlux offices.
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A.F.F. conceived the study with input from B.P. A.F.F. conducted the analysis and wrote the initial paper. A.G.K., P.G., J.J., A.C. and B.P. provided guidance on the methods throughout the analysis. M.A., L.W., W.K.S. and J.A.B. provided guidance in part on methods and mainly on the interpretation of results. All authors contributed substantial revisions to the text and figures.
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Extended data figures and tables
Extended Data Fig. 1 Across historical simulations and projections, rainfall is becoming less frequent, but more intense.
Historical and projected rainfall trends of (a, b) wet day frequency, and (c, d) wet day intensity, and (e, f) annual rainfall total using CMIP6 historical simulations (1940–2020) and CMIP6 RCP8.5 models (2020–2099).
Extended Data Fig. 2 Across observation-based rainfall datasets, rainfall is becoming less frequent, but more intense.
Rainfall trends of (a, b) wet day frequency, and (c, d) wet day intensity, and (e, f) annual rainfall total using CPC gridded observations (1980–2020) and MERRA2 model reanalysis (1980–2020).
Extended Data Fig. 3 Wet day frequency and annual rainfall amount have enough uncorrelated information to be included together and partitioned in a regression.
(a) Variance inflation factor of wet day frequency and intensity. Higher values (especially much over 5) indicate multi-collinearity with annual rainfall mean and thus higher uncertainty partitioning effects between the variables. (b) Interannual coefficient of variation computed as the interannual standard deviation divided by interannual mean for each respective rainfall characteristic. Similar magnitudes between variables suggest variability of one variable is not dominating the regression.
Extended Data Fig. 4 Mechanistic explanation of vegetation sensitivity to more intense, less frequent wet days across the global mean rainfall gradient (in Fig. 3).
(a) Effect of soil, plant, and atmospheric factors on vegetation sensitivity to more intense, less frequent wet days. ** indicates significance (p < 0.05). Positive values suggest that increasing the respective driver promotes higher vegetation behavior in years with more intense, less frequent wet days. Computation of individual mechanistic factors is discussed in the Methods and their relationships with mean annual rainfall are shown in Fig. S15. Mean VPD, Soil Moisture, and Solar Radiation “Sensitivity” refers to the response of these climate variables to more intense, less frequent wet days (see text and Methods). (b) Variance explained of factors in (a).
Extended Data Fig. 5 Empirically estimated vegetation trends due to daily rainfall variability trends.
Spatial maps of empirically estimated vegetation trends due to trends in daily rainfall variability from (a) CPC, (b) MERRA2, (c) CMIP6 historical simulations, and (d) CMIP6 RCP8.5 projections.
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This file includes one notes section that covers several details about robustness of the results in the main text. Supplementary Figs. 1–20 provide robustness tests and context to Figs. 1, 3 and 4. Supplementary Tables 1 and 2 include details about the CMIP6 models and FLUXNET sites.
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Feldman, A.F., Konings, A.G., Gentine, P. et al. Large global-scale vegetation sensitivity to daily rainfall variability. Nature 636, 380–384 (2024). https://doi.org/10.1038/s41586-024-08232-z
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DOI: https://doi.org/10.1038/s41586-024-08232-z
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