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Northern ecosystem productivity reduced by Rossby-wave-driven hot–dry conditions

Abstract

Large-scale quasi-stationary Rossby waves in the tropospheric jet stream favour spatially compounding hot–dry and cold–wet weather across the northern hemisphere. However, how this circumglobal circulation pattern affects northern hemisphere ecosystem productivity remains unexplored. Here, using satellite proxies of vegetation photosynthesis, we assess the impact of Rossby wave-7 events during which the jet stream exhibits seven peaks and troughs and tends to produce prolonged weather anomalies. Our results show organized declines in vegetation productivity in warm cores and enhancement in cold cores at northern mid-latitudes during summer Rossby wave-7 events. Mid-latitude biomes within warm cores become much more susceptible to water limitations, resulting from an increased exposure to compound hot–dry (or cold–wet) extremes and a nonlinear physiological response to compound stressors. Of the warm cores analysed, wave events elevate the climatic risk of productivity declines by a factor of 8.3, 6.2 and 4.0 over western Europe, western Asia and the western United States, respectively, due to hot–dry extremes. In particular, 32–44% of the warm anomalies and 52–88% of the dry anomalies fall within the range of warmer–drier conditions projected for 2081–2100 by state-of-the-art climate models under a medium emissions scenario. Therefore, the observed Rossby-wave-driven impacts provide an indication of how a warmer–drier future climate could reduce the carbon uptake capacity of northern hemisphere ecosystems.

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Fig. 1: Regionally averaged productivity anomalies during RW7 events.
Fig. 2: The dependence of vegetation productivity on SM.
Fig. 3: Productivity anomalies during compound RW7 events.
Fig. 4: Productivity response to joint occurrences of Ta and SM extremes.
Fig. 5: AIF for hot–dry and cold–wet extremes during RW7 events.
Fig. 6: RW7-observed Ta and SM anomalies versus projected future Ta and SM changes.

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Data availability

All observational data that support the findings of this study are available as follows. The MODIS fPAR data are available at https://e4ftl01.cr.usgs.gov/MOLT/MOD15A2H.061/. MODIS surface reflectance data for deriving NIRV are available at https://e4ftl01.cr.usgs.gov/MOTA/MCD43C4.061/. The ERA5 reanalysis product is available at https://cds.climate.copernicus.eu/datasets/reanalysis-era5-single-levels?tab=overview. The ERA5-land reanalysis product is available at https://cds.climate.copernicus.eu/datasets/reanalysis-era5-land?tab=overview. The CSIF data are available at https://osf.io/8xqy6/. The Breathing Earth System Simulator PAR data are available at https://www.environment.snu.ac.kr/data/. The CMIP6 ESM outputs are available at https://esgf-node.ipsl.upmc.fr/search/cmip6-ipsl/.

Code availability

All data analyses and visualizations were performed using MATLAB 2024b. The processing codes are available from the corresponding author upon request.

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Acknowledgements

X.L. and P.G. acknowledge support from the LEMONTREE (Land Ecosystem Models based on New Theory, obseRvations and ExperimEnts) project, funded through the generosity of E. and W. Schmidt by recommendation of the Schmidt Futures programme. This work is supported by the high-performance computing platform of Peking University.

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X.L. and P.G. designed the research. X.L. and Y.L. performed analysis and drafted the paper. X.L., Y.L., J.L., K.K. and P.G. contributed to the interpretation of the results and to the text.

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Correspondence to Xu Lian.

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Nature Geoscience thanks Yangjian Zhang and the other, anonymous, reviewer(s) for their contribution to the peer review of this work. Primary Handling Editor: Tom Richardson, in collaboration with the Nature Geoscience team

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Lian, X., Li, Y., Liu, J. et al. Northern ecosystem productivity reduced by Rossby-wave-driven hot–dry conditions. Nat. Geosci. 18, 615–623 (2025). https://doi.org/10.1038/s41561-025-01722-3

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