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51. Disentangling the contributions of anthropogenic climate change, greenhouse gases, and aerosols to heat-related mortality in Great Britain: a climate change impact attribution study K. Wan et al. 10.1016/S2542-5196(25)00050-6
52. Anthropogenic influence has intensified the severity of summer compound hot and drought events over xinjiang, China X. Zhang et al. 10.1016/j.wace.2025.100774
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55. Differences and similarities in Indian monsoon response to aerosols and to land-use/land-cover change R. Puri & A. Giannini 10.1088/1748-9326/adcc43
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58. Arctic amplification–induced decline in West and South Asia dust warrants stronger antidesertification toward carbon neutrality F. Wang et al. 10.1073/pnas.2317444121
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60. Estimating centennial-scale changes in global terrestrial near-surface wind speed based on CMIP6 GCMs C. Shen et al. 10.1088/1748-9326/ac1378
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63. Human contribution to atmosphere-ocean thermodynamic factors affecting the intense tropical cyclones over the Arabian Sea during the post-monsoon season A. Pathaikara et al. 10.1016/j.wace.2025.100755
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65. Frequency of the winter temperature extremes over Siberia dominated by the Atlantic Meridional Overturning Circulation H. Wang et al. 10.1038/s41612-022-00307-w
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67. Attributing observed permafrost warming in the northern hemisphere to anthropogenic climate change L. Gudmundsson et al. 10.1088/1748-9326/ac8ec2
68. Future increases in Amazonia water stress from CO2 physiology and deforestation Y. Li et al. 10.1038/s44221-023-00128-y
69. Neutral Mode Dominates the Forced Global and Regional Surface Temperature Response in the Past and Future F. Liu et al. 10.1029/2022GL098788
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71. Quantifying contributions of natural variability and anthropogenic forcings on increased fire weather risk over the western United States Y. Zhuang et al. 10.1073/pnas.2111875118
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80. Hemispheric-wide climate response to regional COVID-19-related aerosol emission reductions: the prominent role of atmospheric circulation adjustments N. Fahrenbach & M. Bollasina 10.5194/acp-23-877-2023
81. The magnitude of climate change-induced migration: an overview of projections and a case for attribution J. Schewe & R. Beyer 10.3389/fclim.2025.1570995
82. Reversed impacts of the Arctic oscillation on the precipitation over the South China Sea and its surrounding areas in October and November T. Dong et al. 10.1007/s00382-020-05461-6
83. Detectable Anthropogenic Intensification of the Summer Compound Hot and Dry Events Over Global Land Areas R. Pan et al. 10.1029/2022EF003254
84. Evaluation of CNRM Earth System Model, CNRM‐ESM2‐1: Role of Earth System Processes in Present‐Day and Future Climate R. Séférian et al. 10.1029/2019MS001791
85. Quantification of human contribution to soil moisture-based terrestrial aridity Y. Wang et al. 10.1038/s41467-022-34071-5
86. Amplification of the Temperature Seasonality in the Mediterranean Region Under Anthropogenic Climate Change X. Feng et al. 10.1029/2022GL099658
87. Attribution of the Record‐Breaking Extreme Precipitation Events in July 2021 Over Central and Eastern China to Anthropogenic Climate Change L. Wang et al. 10.1029/2023EF003613
88. Historical global ocean wave data simulated with CMIP6 anthropogenic and natural forcings A. Patra et al. 10.1038/s41597-023-02228-6
89. Experiment design of the International CLIVAR C20C+ Detection and Attribution project D. Stone et al. 10.1016/j.wace.2019.100206
90. CMIP6 captures the satellite-era jet slowdown and Arctic amplification, yet projects future jet speedup and tropical amplification R. Robinson et al. 10.1007/s00382-023-06839-y
91. Future greening of the Earth may not be as large as previously predicted Q. Zhao et al. 10.1016/j.agrformet.2020.108111
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97. Improved Decadal Predictions of North Atlantic Subpolar Gyre SST in CMIP6 L. Borchert et al. 10.1029/2020GL091307
98. Unleashing the power of the Sun: the increasing impact of the solar cycle on off-season super typhoons since the 1990s C. Wu et al. 10.1038/s41612-023-00495-z
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101. Human driven climate change increased the likelihood of the 2023 record area burned in Canada M. Kirchmeier-Young et al. 10.1038/s41612-024-00841-9
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