322 citations as recorded by crossref.

1. Breakdown of NAO reproducibility into internal versus externally-forced components: a two-tier pilot study H. Douville et al. 10.1007/s00382-018-4141-3
2. Drivers of low-frequency Sahel precipitation variability: comparing CMIP5 and CMIP6 ensemble means with observations R. Herman et al. 10.1007/s00382-023-06755-1
3. Decreasing surface chlorophyll in the tropical ocean as an indicator of anthropogenic greenhouse effect during 1998–2020 F. Tian & R. Zhang 10.1088/1748-9326/ace638
4. Counteracting greenhouse gas and aerosol influences intensify global water seasonality over the past century F. Zhao et al. 10.1038/s43247-025-02025-6
5. Drivers and mechanisms contributing to excess warming in Europe during recent decades B. Dong & R. Sutton 10.1038/s41612-025-00930-3
6. National attribution of historical climate damages C. Callahan & J. Mankin 10.1007/s10584-022-03387-y
7. The burden of heat-related mortality attributable to recent human-induced climate change A. Vicedo-Cabrera et al. 10.1038/s41558-021-01058-x
8. Multi-model event attribution of the summer 2013 heat wave in Korea Y. Kim et al. 10.1016/j.wace.2018.03.004
9. Causes of the long-term variability of southwestern South America precipitation in the IPSL-CM6A-LR model J. Villamayor et al. 10.1007/s00382-021-05811-y
10. Understanding Differences in Event Attribution Results Arising from Modeling Strategy W. Zhang et al. 10.1007/s13351-022-1109-3
11. Amplified warming of North American cold extremes linked to human-induced changes in temperature variability R. Blackport & J. Fyfe 10.1038/s41467-024-49734-8
12. Characteristics of Future Warmer Base States in CESM2 G. Meehl et al. 10.1029/2020EA001296
13. The DOE E3SM Model Version 2: Overview of the Physical Model and Initial Model Evaluation J. Golaz et al. 10.1029/2022MS003156
14. Precipitation regime changes in High Mountain Asia driven by cleaner air J. Jiang et al. 10.1038/s41586-023-06619-y
15. Exploring the value of Dioscorea melanophyma: an orphan crop from China Z. Chen et al. 10.1016/j.indcrop.2024.120136
16. State dependence of CO 2 forcing and its implications for climate sensitivity H. He et al. 10.1126/science.abq6872
17. Understanding pattern scaling errors across a range of emissions pathways C. Wells et al. 10.5194/esd-14-817-2023
18. Exploring the impact of the recent global warming on extreme weather events in Central Asia using the counterfactual climate data ATTRICI v1.1 B. Fallah & M. Rostami 10.1007/s10584-024-03743-0
19. Suppressed Late‐20th Century Warming in CMIP6 Models Explained by Forcing and Feedbacks C. Smith & P. Forster 10.1029/2021GL094948
20. Current and future adaptation potential of heat-tolerant maize in Cameroon: a combined attribution and adaptation study L. Jansen et al. 10.1088/1748-9326/ada459
21. Sensitivity of Glaciers in the European Alps to Anthropogenic Atmospheric Forcings: Case Study of the Argentière Glacier L. Clauzel et al. 10.1029/2022GL100363
22. Anthropogenic influence on extreme temperatures in China based on CMIP6 models T. Hu & Y. Sun 10.1002/joc.7402
23. Impacts of natural and anthropogenic forcings on historical and future changes in global-land surface air temperature in CMIP6–DAMIP simulations C. Xu et al. 10.1007/s10584-024-03686-6
24. Human-induced warming accelerates local evapotranspiration and precipitation recycling over the Tibetan Plateau T. Cheng et al. 10.1038/s43247-024-01563-9
25. Attribution of multi-annual to decadal changes in the climate system: The Large Ensemble Single Forcing Model Intercomparison Project (LESFMIP) D. Smith et al. 10.3389/fclim.2022.955414
26. Weakening of subsurface ocean temperature seasonality over the past four decades F. Liu et al. 10.1038/s43247-024-01986-4
27. Stratocumulus adjustments to aerosol perturbations disentangled with a causal approach E. Fons et al. 10.1038/s41612-023-00452-w
28. Making climate projections conditional on historical observations A. Ribes et al. 10.1126/sciadv.abc0671
29. Attributing heatwave-related mortality to climate change: a case study of the 2009 Victorian heatwave in Australia S. Perkins-Kirkpatrick et al. 10.1088/2752-5295/ada8cd
30. Contributions of internal climate variability in driving global and ocean temperature variations using multi-layer perceptron neural network H. Xiao et al. 10.1016/j.accre.2022.06.001
31. Hadley cell expansion in CMIP6 models K. Grise & S. Davis 10.5194/acp-20-5249-2020
32. Constraining human contributions to observed warming since the pre-industrial period N. Gillett et al. 10.1038/s41558-020-00965-9
33. Copula-based interannual variability of winter–spring hot drought events over the low-latitude highlands of China D. Wen & J. Cao 10.1016/j.jhydrol.2025.132936
34. Robust projection of East Asian summer monsoon rainfall based on dynamical modes of variability D. Xue et al. 10.1038/s41467-023-39460-y
35. Sharp decline of dust events induces regional wetting over arid and semi-arid Northwest China in the NCAR Community atmosphere model X. Xie et al. 10.1088/1748-9326/ad16a5
36. Anthropogenic influence on seasonal extreme temperatures in eastern China at century scale T. Hu et al. 10.1016/j.wace.2024.100675
37. AerChemMIP: quantifying the effects of chemistry and aerosols in CMIP6 W. Collins et al. 10.5194/gmd-10-585-2017
38. The role of anthropogenic aerosols in the anomalous cooling from 1960 to 1990 in the CMIP6 Earth system models J. Zhang et al. 10.5194/acp-21-18609-2021
39. Natural and Anthropogenic Forcing of Multi‐Decadal to Centennial Scale Variability of Sea Surface Temperature in the South China Sea N. Goodkin et al. 10.1029/2021PA004233
40. Potential fire risks in South America under anthropogenic forcing hidden by the Atlantic Multidecadal Oscillation Y. Wang & P. Huang 10.1038/s41467-022-30104-1
41. Documenting numerical experiments in support of the Coupled Model Intercomparison Project Phase 6 (CMIP6) C. Pascoe et al. 10.5194/gmd-13-2149-2020
42. Aerosol‐Forced AMOC Changes in CMIP6 Historical Simulations M. Menary et al. 10.1029/2020GL088166
43. Using Climate Model Simulations to Constrain Observations B. Santer et al. 10.1175/JCLI-D-20-0768.1
44. Anthropogenic Aerosol Dominates the Decadal Change in Evapotranspiration over Southeastern China in the Past Four Decades Z. Kong et al. 10.3390/rs17030561
45. High Flux of Small Sulfate Aerosols During the 1970s Reconstructed From the SE‐Dome Ice Core in Greenland Y. Iizuka et al. 10.1029/2022JD036880
46. Constraining the entire Earth system projections for more reliable climate change adaptation planning C. Li et al. 10.1126/sciadv.adr5346
47. A New Emergent Constraint Corrected Projections of Indian Summer Monsoon Rainfall P. Rajesh & B. Goswami 10.1029/2021GL096671
48. Attributing and Projecting Heatwaves Is Hard: We Can Do Better G. Van Oldenborgh et al. 10.1029/2021EF002271
49. 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
50. Evaluation and attribution of historical surface air temperature changes over China simulated by coupled and uncoupled models L. Zuo et al. 10.3389/feart.2022.1061369
51. Reconstructed temperature change in late summer over the eastern Tibetan Plateau since 1867 CE and the role of anthropogenic forcing H. Yin et al. 10.1016/j.gloplacha.2021.103715
52. ACCESS datasets for CMIP6: methodology and idealised experiments C. Mackallah et al. 10.1071/ES21031
53. Contributions of external forcing and internal variability to the multidecadal warming rate of East Asia in the present and future climate D. Jeong et al. 10.1038/s41612-024-00573-w
54. Arctic amplification–induced decline in West and South Asia dust warrants stronger antidesertification toward carbon neutrality F. Wang et al. 10.1073/pnas.2317444121
55. Estimating centennial-scale changes in global terrestrial near-surface wind speed based on CMIP6 GCMs C. Shen et al. 10.1088/1748-9326/ac1378
56. Attribution of the unprecedented summer 2022 compound marine and terrestrial heatwave in the Northwest Pacific Q. Chen et al. 10.1088/1748-9326/ad5ab0
57. Attributing the Decline of Evapotranspiration over the Asian Monsoon Region during the Period 1950–2014 in CMIP6 Models X. Zhu et al. 10.3390/rs16112027
58. 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
59. 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
60. Seasonal advance of intense tropical cyclones in a warming climate K. Shan et al. 10.1038/s41586-023-06544-0
61. Attributing observed permafrost warming in the northern hemisphere to anthropogenic climate change L. Gudmundsson et al. 10.1088/1748-9326/ac8ec2
62. Future increases in Amazonia water stress from CO2 physiology and deforestation Y. Li et al. 10.1038/s44221-023-00128-y
63. Neutral Mode Dominates the Forced Global and Regional Surface Temperature Response in the Past and Future F. Liu et al. 10.1029/2022GL098788
64. Stronger Arctic amplification from anthropogenic aerosols than from greenhouse gases Y. Wu et al. 10.1038/s41612-024-00696-0
65. 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
66. Aerosols overtake greenhouse gases causing a warmer climate and more weather extremes toward carbon neutrality P. Wang et al. 10.1038/s41467-023-42891-2
67. Global warming at near-constant tropospheric relative humidity is supported by observations H. Douville et al. 10.1038/s43247-022-00561-z
68. Influence of Stratospheric Ozone Changes on Stratospheric Temperature Trends in Recent Decades L. Zhou et al. 10.3390/rs14215364
69. Higher Sensitivity of Northern Hemisphere Monsoon to Anthropogenic Aerosol Than Greenhouse Gases J. Cao et al. 10.1029/2022GL100270
70. Uniformly elevated future heat stress in China driven by spatially heterogeneous water vapor changes F. Wang et al. 10.1038/s41467-024-48895-w
71. Human influence can explain the widespread exceptional warmth in 2023 S. Min 10.1038/s43247-024-01391-x
72. Model inter-comparison design for large-scale water quality models M. van Vliet et al. 10.1016/j.cosust.2018.10.013
73. 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
74. 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
75. Detectable Anthropogenic Intensification of the Summer Compound Hot and Dry Events Over Global Land Areas R. Pan et al. 10.1029/2022EF003254
76. 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
77. Quantification of human contribution to soil moisture-based terrestrial aridity Y. Wang et al. 10.1038/s41467-022-34071-5
78. Amplification of the Temperature Seasonality in the Mediterranean Region Under Anthropogenic Climate Change X. Feng et al. 10.1029/2022GL099658
79. 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
80. Historical global ocean wave data simulated with CMIP6 anthropogenic and natural forcings A. Patra et al. 10.1038/s41597-023-02228-6
81. Experiment design of the International CLIVAR C20C+ Detection and Attribution project D. Stone et al. 10.1016/j.wace.2019.100206
82. 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
83. Future greening of the Earth may not be as large as previously predicted Q. Zhao et al. 10.1016/j.agrformet.2020.108111
84. Intensifying human-driven heatwaves characteristics and heat related mortality over Africa P. Adigun et al. 10.1088/2752-5295/ad1f41
85. Significant impact of forcing uncertainty in a large ensemble of climate model simulations J. Fyfe et al. 10.1073/pnas.2016549118
86. Recent decades witness a strong east-west gradient of monsoon precipitation changes over Northern India A. Kumari et al. 10.1016/j.atmosres.2025.108014
87. Detection and Attribution of Changes in Summer Compound Hot and Dry Events over Northeastern China with CMIP6 Models W. Li et al. 10.1007/s13351-022-1112-8
88. An overview of the E3SM version 2 large ensemble and comparison to other E3SM and CESM large ensembles J. Fasullo et al. 10.5194/esd-15-367-2024
89. Improved Decadal Predictions of North Atlantic Subpolar Gyre SST in CMIP6 L. Borchert et al. 10.1029/2020GL091307
90. 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
91. Anthropogenic Attribution of the Increasing Seasonal Amplitude in Surface Ocean pCO2 F. Joos et al. 10.1029/2023GL102857
92. Reconstruction of hourly coastal water levels and counterfactuals without sea level rise for impact attribution S. Treu et al. 10.5194/essd-16-1121-2024
93. 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
94. Efficacy of climate forcings in transient CMIP6 simulations G. Myhre et al. 10.3389/fclim.2024.1397358
95. Modifying emissions scenario projections to account for the effects of COVID-19: protocol for CovidMIP R. Lamboll et al. 10.5194/gmd-14-3683-2021
96. Anthropogenic Aerosols, Greenhouse Gases, and the Uptake, Transport, and Storage of Excess Heat in the Climate System D. Irving et al. 10.1029/2019GL082015
97. Mitigation needed to avoid unprecedented multi-decadal North Atlantic Oscillation magnitude D. Smith et al. 10.1038/s41558-025-02277-2
98. Spatially Resolved Temperature Response Functions to CO2 Emissions L. Freese et al. 10.1029/2024GL108788
99. Towards operational predictions of the near-term climate Y. Kushnir et al. 10.1038/s41558-018-0359-7
100. A novel statistical decomposition of the historical change in global mean surface temperature G. Qian et al. 10.1088/1748-9326/abea34
101. Accelerated increases in global and Asian summer monsoon precipitation from future aerosol reductions L. Wilcox et al. 10.5194/acp-20-11955-2020
102. The vertical profile of recent tropical temperature trends: Persistent model biases in the context of internal variability D. Mitchell et al. 10.1088/1748-9326/ab9af7
103. Compound droughts and hot extremes: Characteristics, drivers, changes, and impacts Z. Hao et al. 10.1016/j.earscirev.2022.104241
104. Volcanically forced Madden–Julian oscillation triggers the immediate onset of El Niño H. Kim et al. 10.1038/s41467-025-56692-2
105. Highest ocean heat in four centuries places Great Barrier Reef in danger B. Henley et al. 10.1038/s41586-024-07672-x
106. Anthropogenic influence on the extremely low September sea ice and hot summer of 2020 over the Arctic and its future risk of occurrence K. Wang et al. 10.1016/j.wace.2024.100674
107. Past and future response of the North Atlantic warming hole to anthropogenic forcing S. Qasmi 10.5194/esd-14-685-2023
108. The emergence of anthropogenic signal in mean and extreme precipitation trend over China by using two large ensembles W. Li et al. 10.1088/1748-9326/abd26d
109. A framework for detection and attribution of regional precipitation change: Application to the United States historical record M. Risser et al. 10.1007/s00382-022-06321-1
110. Anthropogenic sulfate-climate interactions suppress dust activity over East Asia X. Xie et al. 10.1038/s43247-025-02147-x
111. One-third of the global soybean production failure in 2012 is attributable to climate change R. Hamed et al. 10.1038/s43247-025-02171-x
112. Improving the Estimation of Human Climate Influence by Selecting Appropriate Forcing Simulations C. Li et al. 10.1029/2021GL095500
113. The Meteorological Research Institute Earth System Model Version 2.0, MRI-ESM2.0: Description and Basic Evaluation of the Physical Component S. YUKIMOTO et al. 10.2151/jmsj.2019-051
114. The burden of heatwave-related preterm births and associated human capital losses in China Y. Zhang et al. 10.1038/s41467-022-35008-8
115. Fire carbon emissions over Equatorial Asia reduced by shortened dry seasons S. Wang et al. 10.1038/s41612-023-00455-7
116. Impacts of anthropogenic climate change on meteorological drought in China R. Dai et al. 10.3389/feart.2024.1369523
117. Evaluation of climate variability and change in ACCESS historical simulations for CMIP6 H. Rashid et al. 10.1071/ES21028
118. Attributing observed increase in extreme precipitation in China to human influence S. Dong et al. 10.1088/1748-9326/ac888e
119. A Recent Systematic Increase in Vapor Pressure Deficit over Tropical South America A. Barkhordarian et al. 10.1038/s41598-019-51857-8
120. Multifaceted aerosol effects on precipitation P. Stier et al. 10.1038/s41561-024-01482-6
121. Seasonal to Decadal Predictions With MIROC6: Description and Basic Evaluation T. Kataoka et al. 10.1029/2019MS002035
122. Scenario setup and forcing data for impact model evaluation and impact attribution within the third round of the Inter-Sectoral Impact Model Intercomparison Project (ISIMIP3a) K. Frieler et al. 10.5194/gmd-17-1-2024
123. Counterbalancing influences of aerosols and greenhouse gases on atmospheric rivers S. Baek & J. Lora 10.1038/s41558-021-01166-8
124. Attribution of global lake systems change to anthropogenic forcing L. Grant et al. 10.1038/s41561-021-00833-x
125. Anthropogenic forcing decreases the probability of the 2020 Yangtze River extreme flood and future risk X. Li et al. 10.1016/j.atmosres.2024.107662
126. Flipping of temperature and precipitation trends over the Indian subcontinent due to diametrically opposing influence of GHGs and aerosols A. Shilin et al. 10.1088/1748-9326/ad4974
127. Determining the Anthropogenic Greenhouse Gas Contribution to the Observed Intensification of Extreme Precipitation S. Paik et al. 10.1029/2019GL086875
128. Stratospheric ozone depletion and tropospheric ozone increases drive Southern Ocean interior warming W. Liu et al. 10.1038/s41558-022-01320-w
129. Distinct anthropogenic aerosol and greenhouse gas effects on El Niño/Southern Oscillation variability X. Ren & W. Liu 10.1038/s43247-025-01996-w
130. Nonlinearity of the cloud response postpones climate penalty of mitigating air pollution in polluted regions H. Jia & J. Quaas 10.1038/s41558-023-01775-5
131. Detection and Attribution of Climate Change Using a Neural Network C. Bône et al. 10.1029/2022MS003475
132. Impact of industrial versus biomass burning aerosols on the Atlantic Meridional Overturning Circulation R. Allen et al. 10.1038/s41612-024-00602-8
133. Evidence of human influence on Northern Hemisphere snow loss A. Gottlieb & J. Mankin 10.1038/s41586-023-06794-y
134. Estimating the burden of temperature-related low birthweight attributable to anthropogenic climate change in low-income and middle-income countries: a retrospective, multicentre, epidemiological study Z. Zhu et al. 10.1016/S2542-5196(24)00242-0
135. The PMIP4 contribution to CMIP6 – Part 1: Overview and over-arching analysis plan M. Kageyama et al. 10.5194/gmd-11-1033-2018
136. Reconciling roles of sulphate aerosol forcing and internal variability in Atlantic multidecadal climate changes M. Watanabe & H. Tatebe 10.1007/s00382-019-04811-3
137. The fate of Holoregmia, a monospecific genus endemic to the Brazilian Caatinga, under different future climate scenarios T. Rabelo-Costa et al. 10.5091/plecevo.90511
138. Half a degree additional warming, prognosis and projected impacts (HAPPI): background and experimental design D. Mitchell et al. 10.5194/gmd-10-571-2017
139. Assessment of Chinese suitable habitats of Zanthoxylum nitidum in different climatic conditions by Maxent model, HPLC, and chemometric methods Y. Yang et al. 10.1016/j.indcrop.2023.116515
140. Drivers of Recent North Pacific Decadal Variability: The Role of Aerosol Forcing A. Dittus et al. 10.1029/2021EF002249
141. The impact of long-term memory on the climate response to greenhouse gas emissions N. Yuan et al. 10.1038/s41612-022-00298-8
142. The Influence of Natural and Anthropogenic Forcing on Water and Energy Balance and on Photosynthesis J. Song et al. 10.3390/land10111151
143. Anthropogenic aerosol effects on tropospheric circulation and sea surface temperature (1980–2020): separating the role of zonally asymmetric forcings C. Diao et al. 10.5194/acp-21-18499-2021
144. Detection and attribution of extreme precipitation events over the Asian monsoon region T. Dong et al. 10.1016/j.wace.2022.100497
145. Recent decadal weakening of the summer Eurasian westerly jet attributable to anthropogenic aerosol emissions B. Dong et al. 10.1038/s41467-022-28816-5
146. Human-induced intensified seasonal cycle of sea surface temperature F. Liu et al. 10.1038/s41467-024-48381-3
147. Tropical eastern Pacific cooling trend reinforced by human activity E. Chung et al. 10.1038/s41612-024-00713-2
148. The Climate Response to Emissions Reductions Due to COVID‐19: Initial Results From CovidMIP C. Jones et al. 10.1029/2020GL091883
149. Description of historical and future projection simulations by the global coupled E3SMv1.0 model as used in CMIP6 X. Zheng et al. 10.5194/gmd-15-3941-2022
150. Influence of anthropogenic forcing on the long‐range correlation of air temperature in China Y. Mei et al. 10.1002/joc.7914
151. The Polar Amplification Model Intercomparison Project (PAMIP) contribution to CMIP6: investigating the causes and consequences of polar amplification D. Smith et al. 10.5194/gmd-12-1139-2019
152. Radiative effects of reduced aerosol emissions during the COVID-19 pandemic and the future recovery S. Fiedler et al. 10.1016/j.atmosres.2021.105866
153. Bias in CMIP6 models as compared to observed regional dimming and brightening K. Moseid et al. 10.5194/acp-20-16023-2020
154. Effects of Anthropogenic Forcings on Multidecadal Variability of the Sea Level Around the Japanese Coast Simulated by MRI‐ESM2.0 for CMIP6 Y. Ushijima et al. 10.1029/2022GL099987
155. Internal Variability Dominates Over Externally Forced Ocean Circulation Changes Seen Through CFCs J. Lester et al. 10.1029/2020GL087585
156. Seasonally distinct contributions of greenhouse gases and anthropogenic aerosols to historical changes in Arctic moisture budget H. Choi et al. 10.1038/s41612-023-00518-9
157. Modeling seasonal trends in optimum temperatures over India N. Agrawal et al. 10.2166/wcc.2020.072
158. Skilful decadal predictions of subpolar North Atlantic SSTs using CMIP model-analogues M. Menary et al. 10.1088/1748-9326/ac06fb
159. Detection and attribution of summer temperature changes in China during the last millennium Z. Wang et al. 10.1002/joc.7595
160. Anthropogenic Influence on Decadal Changes in Concurrent Hot and Dry Events over China around the Mid-1990s Q. Su et al. 10.1007/s00376-023-2319-z
161. Distinct Influences of Land Cover and Land Management on Seasonal Climate D. Singh et al. 10.1029/2018JD028874
162. CMIP6 simulations with the compact Earth system model OSCAR v3.1 Y. Quilcaille et al. 10.5194/gmd-16-1129-2023
163. Consistent Trends in Dry Spell Length in Recent Observations and Future Projections C. Wainwright et al. 10.1029/2021GL097231
164. Uncertainty in Simulating Twentieth Century West African Precipitation Trends: The Role of Anthropogenic Aerosol Emissions P. Monerie et al. 10.1029/2022EF002995
165. Globally unequal effect of extreme heat on economic growth C. Callahan & J. Mankin 10.1126/sciadv.add3726
166. Past variations and future projection of runoff in typical basins in 10 water zones, China X. Guan et al. 10.1016/j.scitotenv.2021.149277
167. Aerosol absorption has an underappreciated role in historical precipitation change B. Samset 10.1038/s43247-022-00576-6
168. Increasing 2020‐Like Boreal Summer Rainfall Extremes Over Northeast Indian Subcontinent Under Greenhouse Warming H. Tang et al. 10.1029/2021GL096377
169. Assessment of suitable cultivation region for Panax notoginseng under different climatic conditions using MaxEnt model and high-performance liquid chromatography in China P. Zhan et al. 10.1016/j.indcrop.2021.114416
170. Physical processes of summer extreme rainfall interannual variability in Eastern China—part II: evaluation of CMIP6 models N. Freychet et al. 10.1007/s00382-022-06137-z
171. Observationally-constrained projections of an ice-free Arctic even under a low emission scenario Y. Kim et al. 10.1038/s41467-023-38511-8
172. Strong large-scale climate response to North American sulphate aerosols in CESM I. García-Martínez et al. 10.1088/1748-9326/abbe45
173. The dynamic and thermodynamic processes dominating the reduction of global land monsoon precipitation driven by anthropogenic aerosols emission T. Zhou et al. 10.1007/s11430-019-9613-9
174. 21st Century Scenario Forcing Increases More for CMIP6 Than CMIP5 Models H. Fredriksen et al. 10.1029/2023GL102916
175. The effect of experiment conditioning on estimates of human influence on extreme weather D. Stone et al. 10.1016/j.wace.2022.100427
176. Observational Constraint on the Contributions of Greenhouse Gas Emission and Anthropogenic Aerosol Removal to Tibetan Plateau Future Warming J. Jiang & T. Zhou 10.1029/2023GL105427
177. Anthropogenic influence on altitudinally amplified temperature change in the Tibetan Plateau Y. Sun et al. 10.1088/1748-9326/ad3bd3
178. Evaluation of the environmental factors influencing the quality of Astragalus membranaceus var. mongholicus based on HPLC and the Maxent model P. Dong et al. 10.1186/s12870-024-05355-3
179. Human influences on spatially compounding flooding and heatwave events in China and future increasing risks C. Qian et al. 10.1016/j.wace.2023.100616
180. An updated assessment of past and future warming over France based on a regional observational constraint A. Ribes et al. 10.5194/esd-13-1397-2022
181. The CMIP6 Data Request (DREQ, version 01.00.31) M. Juckes et al. 10.5194/gmd-13-201-2020
182. Emerging Asian aerosol patterns B. Samset et al. 10.1038/s41561-019-0424-5
183. Observed poleward freshwater transport since 1970 T. Sohail et al. 10.1038/s41586-021-04370-w
184. MIROC6 Large Ensemble (MIROC6-LE): experimental design and initial analyses H. Shiogama et al. 10.5194/esd-14-1107-2023
185. Attributing the recent weakening of the South Asian subtropical westerlies P. Upadhyaya et al. 10.1038/s41612-024-00777-0
186. Transition from positive to negative indirect CO2 effects on the vegetation carbon uptake Z. Chen et al. 10.1038/s41467-024-45957-x
187. Human‐Induced Rainfall Reduction in Drought‐Prone Northern Central Asia J. Jiang & T. Zhou 10.1029/2020GL092156
188. Increase in ocean-onto-land droughts and their drivers under anthropogenic climate change Y. Guan et al. 10.1038/s41612-023-00523-y
189. Diurnally asymmetric cloud cover trends amplify greenhouse warming H. Luo et al. 10.1126/sciadv.ado5179
190. Aerosol Forcing Masks and Delays the Formation of the North Atlantic Warming Hole by Three Decades G. Dagan et al. 10.1029/2020GL090778
191. Attribution of historical extreme heat events in different climate zones of China Y. Zhang & Y. Sun 10.1088/1748-9326/adb2a8
192. Detection and attribution of climate change: A deep learning and variational approach C. Bône et al. 10.1017/eds.2022.17
193. Attributing changes in food insecurity to a changing climate S. Dasgupta & E. Robinson 10.1038/s41598-022-08696-x
194. Rapidly increasing likelihood of exceeding 50 °C in parts of the Mediterranean and the Middle East due to human influence N. Christidis et al. 10.1038/s41612-023-00377-4
195. Using historical temperature to constrain the climate sensitivity, the transient climate response, and aerosol-induced cooling O. Morgenstern 10.5194/acp-24-8105-2024
196. Projection of Long‐Term Climate Change in China Under COVID‐19 Recovery Emission Scenarios C. Tian et al. 10.1029/2023JD039197
197. The need for carbon-emissions-driven climate projections in CMIP7 B. Sanderson et al. 10.5194/gmd-17-8141-2024
198. Emergent constraints on future extreme precipitation intensification: from global to continental scales S. Paik et al. 10.1016/j.wace.2023.100613
199. Equatorward shift of the boreal summer intertropical convergence zone in Maritime Continent and the impacts on surface black carbon concentration and public health T. Huang et al. 10.1038/s41612-024-00593-6
200. Fractional change of scattering and absorbing aerosols contributes to Northern Hemisphere Hadley circulation expansion T. Ying et al. 10.1126/sciadv.adq9716
201. Interhemispheric Contrasts of Ocean Heat Content Change Reveals Distinct Fingerprints of Anthropogenic Climate Forcings J. Shi et al. 10.1029/2023GL102741
202. Understanding the combined effects of global warming and anthropogenic aerosol forcing on the South Asian monsoon D. Ayantika et al. 10.1007/s00382-020-05551-5
203. Record-breaking summer rainfall in the Asia–Pacific region attributed to the strongest Asian westerly jet related to aerosol reduction during COVID-19 X. An et al. 10.1088/1748-9326/acdd84
204. Storyline attribution of human influence on a record-breaking spatially compounding flood-heat event J. Wang et al. 10.1126/sciadv.adi2714
205. Evaluating the long‐term ecohydrological suitability of restoration efforts in a typical watershed of the Loess Plateau M. Sun et al. 10.1002/hyp.14362
206. Reversed and comparable climate impacts from historical anthropogenic aerosol and GHG on global-scale tropical cyclone genesis potential J. Cao et al. 10.1088/1748-9326/ac8c5b
207. Benchmark estimate of the effect of anthropogenic emissions on the ocean surface D. Stone & P. Pall 10.1002/joc.7002
208. Errors in Simple Climate Model Emulations of Past and Future Global Temperature Change L. Jackson et al. 10.1029/2022GL098808
209. The Role of Anthropogenic Aerosol Forcing in the 1850–1985 Strengthening of the AMOC in CMIP6 Historical Simulations J. Robson et al. 10.1175/JCLI-D-22-0124.1
210. Multi-Frequency Analysis of Simulated versus Observed Variability in Tropospheric Temperature G. Pallotta & B. Santer 10.1175/JCLI-D-20-0023.1
211. Contributions of External Forcing and Internal Climate Variability to Changes in the Summer Surface Air Temperature over East Asia J. Zha et al. 10.1175/JCLI-D-21-0577.1
212. Hemisphere-asymmetric tropical cyclones response to anthropogenic aerosol forcing J. Cao et al. 10.1038/s41467-021-27030-z
213. Does Regional Hydroclimate Change Scale Linearly With Global Warming? F. Lehner & S. Coats 10.1029/2021GL095127
214. Human influence increases the likelihood of extremely early cherry tree flowering in Kyoto N. Christidis et al. 10.1088/1748-9326/ac6bb4
215. Indian summer monsoon: Extreme events, historical changes, and role of anthropogenic forcings D. Singh et al. 10.1002/wcc.571
216. Extreme temperatures detection and attribution related to external forcing in Madagascar L. Randriamarolaza et al. 10.1002/joc.8065
217. Crop production losses associated with anthropogenic climate change for 1981–2010 compared with preindustrial levels T. Iizumi et al. 10.1002/joc.5818
218. Attribution of ocean temperature change to anthropogenic and natural forcings using the temporal, vertical and geographical structure R. Bilbao et al. 10.1007/s00382-019-04910-1
219. Anthropogenic impacts on changes in summer extreme precipitation over China during 1961–2014: roles of greenhouse gases and anthropogenic aerosols Y. Guo et al. 10.1007/s00382-022-06453-4
220. Emergent constraints on future precipitation changes H. Shiogama et al. 10.1038/s41586-021-04310-8
221. Unraveling the Arctic Sea Ice Change since the Middle of the Twentieth Century N. Kong & W. Liu 10.3390/geosciences13020058
222. Increased aerosol scattering contributes to the recent monsoon rainfall decrease over the Gangetic Plain T. Ying et al. 10.1016/j.scib.2023.08.052
223. Reductions in atmospheric levels of non-CO2 greenhouse gases explain about a quarter of the 1998-2012 warming slowdown X. Su et al. 10.1038/s43247-024-01723-x
224. The Northwestern Pacific Warming Record in August 2020 Occurred Under Anthropogenic Forcing M. Hayashi et al. 10.1029/2020GL090956
225. Detectable anthropogenic influence on summer compound hot events over China from 1965 to 2014 X. Wang et al. 10.1088/1748-9326/ac4d4e
226. Long-Term Precipitation Changes in the Baiu and Akisame Seasons in Japan over the Past 120 Years (1901–2020) H. ENDO 10.2151/jmsj.2023-019
227. Change from aerosol-driven to cloud-feedback-driven trend in short-wave radiative flux over the North Atlantic D. Grosvenor & K. Carslaw 10.5194/acp-23-6743-2023
228. Indicators of Global Climate Change 2022: annual update of large-scale indicators of the state of the climate system and human influence P. Forster et al. 10.5194/essd-15-2295-2023
229. High‐Resolution CCAM Simulations Over New Zealand and the South Pacific for the Detection and Attribution of Weather Extremes P. Gibson et al. 10.1029/2023JD038530
230. Historical evolution and future trend of Northern Hemisphere snow cover in CMIP5 and CMIP6 models X. Zhu et al. 10.1088/1748-9326/ac0662
231. Human influence on daily temperature variability over land H. Wan et al. 10.1088/1748-9326/ac1cb9
232. Detection and attribution of the summer length changes in the Northern Hemisphere W. Lin & C. Wang 10.1007/s00382-022-06553-1
233. Future Extreme Precipitation in Summer Will Become More Widespread in China Depending on Level of Warming R. Yu et al. 10.1029/2022EF003413
234. Deforestation intensifies daily temperature variability in the northern extratropics J. Ge et al. 10.1038/s41467-022-33622-0
235. Anthropogenic Aerosols Modulated 20th‐Century Sahel Rainfall Variability Via Their Impacts on North Atlantic Sea Surface Temperature S. Zhang et al. 10.1029/2021GL095629
236. Spatio-temporal variations in global surface soil moisture based on multiple datasets: Intercomparison and climate drivers Y. Guan et al. 10.1016/j.jhydrol.2023.130095
237. The 2021 heatwave was less rare in Western Canada than previously thought E. Malinina & N. Gillett 10.1016/j.wace.2024.100642
238. Attribution of summer 2022 extreme wildfire season in Southwest France to anthropogenic climate change M. Lanet et al. 10.1038/s41612-024-00821-z
239. Could detection and attribution of climate change trends be spurious regression? D. Cummins et al. 10.1007/s00382-022-06242-z
240. The Southern Ocean Freshwater Input from Antarctica (SOFIA) Initiative: scientific objectives and experimental design N. Swart et al. 10.5194/gmd-16-7289-2023
241. Anthropogenic influences on the extremely dry and hot summer of 2020 in Southern China and projected changes in the likelihood of the event K. Wang et al. 10.1016/j.wace.2024.100706
242. Evidence of anthropogenic impacts on global drought frequency, duration, and intensity F. Chiang et al. 10.1038/s41467-021-22314-w
243. The extremely hot and dry 2018 summer in central and northern Europe from a multi-faceted weather and climate perspective E. Rousi et al. 10.5194/nhess-23-1699-2023
244. Anthropogenic Aerosols Offsetting Ocean Warming Less Efficiently Since the 1980s T. Sohail et al. 10.1029/2023GL105374
245. Human influence on historical heaviest precipitation events in the Yangtze River Valley Z. Wang et al. 10.1088/1748-9326/acb563
246. The southward shift of hurricane genesis over the northern Atlantic Ocean X. Cao et al. 10.1038/s41612-025-00923-2
247. Climate Sensitivity of GFDL's CM4.0 M. Winton et al. 10.1029/2019MS001838
248. Energy Carbon Emission Reduction Based on Spatiotemporal Heterogeneity: A County-Level Empirical Analysis in Guangdong, Fujian, and Zhejiang Y. Lai et al. 10.3390/su17073218
249. Anthropogenic influence on extreme Meiyu rainfall in 2020 and its future risk T. Zhou et al. 10.1007/s11430-020-9771-8
250. Comparison of the risks and drivers of compound hot-dry and hot-wet extremes in a warming world J. Zeng et al. 10.1088/1748-9326/ad7617
251. Arctic Warming and Associated Sea Ice Reduction in the Early 20th Century Induced by Natural Forcings in MRI‐ESM2.0 Climate Simulations and Multimodel Analyses T. Aizawa et al. 10.1029/2020GL092336
252. Effects of Anthropogenic Aerosol and Greenhouse Gas Emissions on Northern Hemisphere Monsoon Precipitation: Mechanisms and Uncertainty P. Monerie et al. 10.1175/JCLI-D-21-0412.1
253. A study of reanalysis characteristics and evaluation of interdecadal variation of the intensity of South China Sea Summer Monsoon in the early 1990s Z. Zheng et al. 10.1007/s00382-023-07080-3
254. Exceptional stratospheric contribution to human fingerprints on atmospheric temperature B. Santer et al. 10.1073/pnas.2300758120
255. Thermodynamically enhanced precipitation extremes due to counterbalancing influences of anthropogenic greenhouse gases and aerosols Z. Huang et al. 10.1038/s44221-023-00107-3
256. Broader research efforts and assessments needed to uncover the complex climate effects of regional changes in aerosol emissions B. Samset et al. 10.1371/journal.pclm.0000508
257. An uncertain future change in aridity over the tropics P. Monerie et al. 10.1088/1748-9326/ad42b8
258. Quantifying stochastic uncertainty in detection time of human-caused climate signals B. Santer et al. 10.1073/pnas.1904586116
259. Quantification of the Heat-Related Risk and Burden of Hospitalizations for Cause-Specific Injuries and Contribution of Human-Induced Climate Change: A Time-Stratified Case-Crossover Study in China L. Zhou et al. 10.1289/EHP14057
260. Disentangling regional climate change: assessing the contribution of global- and regional-scale anthropogenic factors to observed regional warming A. Barkhordarian 10.1088/1748-9326/ad8f49
261. Attribution of differences in observed warming among subregions of China and observationally constrained projection Y. Dong et al. 10.1002/joc.8322
262. The emerging human influence on the seasonal cycle of sea surface temperature J. Shi et al. 10.1038/s41558-024-01958-8
263. Quantifying the Anthropogenic Greenhouse Gas Contribution to the Observed Spring Snow-Cover Decline Using the CMIP6 Multimodel Ensemble S. Paik & S. Min 10.1175/JCLI-D-20-0002.1
264. Human influence strengthens the contrast between tropical wet and dry regions A. Schurer et al. 10.1088/1748-9326/ab83ab
265. Anthropogenic aerosol impacts on Pacific Coast precipitation in CMIP6 models R. Allen & X. Zhao 10.1088/2752-5295/ac7d68
266. A weather pattern responsible for increasing wildfires in the western United States W. Zhang et al. 10.1088/1748-9326/ad928f
267. A 1 km monthly dataset of historical and future climate changes over China X. Hu et al. 10.1038/s41597-025-04761-y
268. Attribution of extremes to greenhouse gas-induced changes in regional climate variability, distinct from changes in mean climate A. Barkhordarian 10.1088/1748-9326/ad715a
269. Increased Asian aerosols drive a slowdown of Atlantic Meridional Overturning Circulation F. Liu et al. 10.1038/s41467-023-44597-x
270. ClimateBench v1.0: A Benchmark for Data‐Driven Climate Projections D. Watson‐Parris et al. 10.1029/2021MS002954
271. Decoupling of Arctic variability from the North Pacific in a warmer climate S. Jahfer et al. 10.1038/s41612-023-00480-6
272. Distinct anthropogenic greenhouse gas and aerosol induced marine heatwaves X. Ren et al. 10.1088/2752-5295/ad13ac
273. Toward Consistent Observational Constraints in Climate Predictions and Projections G. Hegerl et al. 10.3389/fclim.2021.678109
274. A comparative analysis of the attribution of extreme summer precipitation in south and north parts of the East China monsoon region—with the year 2020 as an example R. Li et al. 10.1002/joc.8260
275. Indo-Pacific warm pool present warming attribution and future projection constraint W. Bai et al. 10.1088/1748-9326/ac5edf
276. Link between the Land–Sea Thermal Contrast and the Asian Summer Monsoon Z. Zuo & K. Zhang 10.1175/JCLI-D-21-0944.1
277. Ocean heat uptake and interbasin redistribution driven by anthropogenic aerosols and greenhouse gases S. Li et al. 10.1038/s41561-023-01219-x
278. Role of anthropogenic forcing and atmospheric circulation in a low-temperature event in February 2022 in eastern China Z. Chen et al. 10.1016/j.accre.2023.11.009
279. ATTRICI v1.1 – counterfactual climate for impact attribution M. Mengel et al. 10.5194/gmd-14-5269-2021
280. Human influence on frequency of temperature extremes T. Hu et al. 10.1088/1748-9326/ab8497
281. Biased Estimates of Equilibrium Climate Sensitivity and Transient Climate Response Derived From Historical CMIP6 Simulations Y. Dong et al. 10.1029/2021GL095778
282. Mechanisms and quantification: How anthropogenic aerosols weaken the East Asian summer monsoon Y. Lang et al. 10.1038/s41612-025-00903-6
283. Attribution of Arctic Sea Ice Decline from 1953 to 2012 to Influences from Natural, Greenhouse Gas, and Anthropogenic Aerosol Forcing B. Mueller et al. 10.1175/JCLI-D-17-0552.1
284. Contributions of Anthropogenic Aerosol Forcing and Multidecadal Internal Variability to Mid‐20th Century Arctic Cooling—CMIP6/DAMIP Multimodel Analysis T. Aizawa et al. 10.1029/2021GL097093
285. Reducing uncertainty in local temperature projections S. Qasmi & A. Ribes 10.1126/sciadv.abo6872
286. Projected drought conditions in Northwest China with CMIP6 models under combined SSPs and RCPs for 2015–2099 S. Li et al. 10.1016/j.accre.2020.09.003
287. Detection, attribution and projection of changes in the extreme temperature range in the Northern Hemisphere X. Feng & C. Qian 10.1016/j.accre.2024.10.006
288. The competition between anthropogenic aerosol and greenhouse gas climate forcing is revealed by North Pacific water-mass changes J. Shi et al. 10.1126/sciadv.adh7746
289. Large Ensemble Simulations of Climate Models for Climate Change Research: A Review P. Lin et al. 10.1007/s00376-024-4012-2
290. Human-induced climate change has decreased wheat production in northern Kazakhstan P. Romanovska et al. 10.1088/2752-5295/ad53f7
291. Are general circulation models obsolete? V. Balaji et al. 10.1073/pnas.2202075119
292. Effects of anthropogenic forcing and atmospheric circulation on the record-breaking welt bulb heat event over southern China in September 2021 D. WANG & Y. SUN 10.1016/j.accre.2022.11.007
293. Responses of compound daytime and nighttime warm-dry and warm-humid events to individual anthropogenic forcings F. Chiang et al. 10.1088/1748-9326/ac80ce
294. Anthropogenic aerosols dominated the decreased solar radiation in eastern China over the last five decades Z. Tang et al. 10.1016/j.jclepro.2022.135150
295. Tropical atlantic climate biases and DAMIP experiments: insights from CMIP6 models P. Silva et al. 10.1007/s00382-024-07253-8
296. Revisiting the reanalysis-model discrepancy in Southern Hemisphere winter storm track trends J. Kang et al. 10.1038/s41612-024-00801-3
297. The GFDL Earth System Model Version 4.1 (GFDL‐ESM 4.1): Overall Coupled Model Description and Simulation Characteristics J. Dunne et al. 10.1029/2019MS002015
298. Spatiotemporal characteristics of the time of emergence for anthropogenic tropospheric temperature changes based on the CMIP6 multi-model results S. Zhang et al. 10.1088/1748-9326/ad34e6
299. The PMIP4 contribution to CMIP6 – Part 3: The last millennium, scientific objective, and experimental design for the PMIP4 past1000 simulations J. Jungclaus et al. 10.5194/gmd-10-4005-2017
300. Global-scale future climate projections from ACCESS model contributions to CMIP6 S. Schroeter et al. 10.1071/ES23029
301. Recent marine heatwaves in the North Pacific warming pool can be attributed to rising atmospheric levels of greenhouse gases A. Barkhordarian et al. 10.1038/s43247-022-00461-2
302. Evaluation of extreme precipitation over Asia in CMIP6 models T. Dong & W. Dong 10.1007/s00382-021-05773-1
303. Unprecedented Heatwave in Western North America during Late June of 2021: Roles of Atmospheric Circulation and Global Warming C. Wang et al. 10.1007/s00376-022-2078-2
304. Detecting Relationship between the North–South Difference in Extreme Precipitation and Solar Cycle in China J. Liu et al. 10.3390/atmos15020175
305. Modern anthropogenic drought in Central Brazil unprecedented during last 700 years N. Stríkis et al. 10.1038/s41467-024-45469-8
306. Anthropogenic emissions and land use/cover change contributions to extreme temperature changes over China W. Xu et al. 10.1016/j.atmosres.2023.106845
307. Enhanced global carbon cycle sensitivity to tropical temperature linked to internal climate variability N. Li et al. 10.1126/sciadv.adl6155
308. Greenhouse warming and anthropogenic aerosols synergistically reduce springtime rainfall in low-latitude East Asia Y. Ryu & S. Min 10.1038/s41612-022-00295-x
309. Influence of anthropogenic and natural forcings on future changes in precipitation projected by the CMIP6–DAMIP models Y. Wang et al. 10.1002/joc.8064
310. Consistency of global carbon budget between concentration- and emission-driven historical experiments simulated by CMIP6 Earth system models and suggestions for improved simulation of CO2 concentration T. Hajima et al. 10.5194/bg-22-1447-2025
311. A dynamical adjustment perspective on extreme event attribution L. Terray 10.5194/wcd-2-971-2021
312. Detection and attribution for land surface air temperature warming in China based on a perfect model selection analysis of optimal fingerprint strategy Z. Guo et al. 10.1007/s00704-024-04966-y
313. Anthropogenic amplification of precipitation variability over the past century W. Zhang et al. 10.1126/science.adp0212
314. Anthropogenic intensification of Arctic anticyclonic circulation Z. Liu et al. 10.1126/sciadv.ads4508
315. The Scenario Model Intercomparison Project (ScenarioMIP) for CMIP6 B. O'Neill et al. 10.5194/gmd-9-3461-2016
316. The Dynamics and Variability Model Intercomparison Project (DynVarMIP) for CMIP6: assessing the stratosphere–troposphere system E. Gerber & E. Manzini 10.5194/gmd-9-3413-2016
317. Time‐Evolving Radiative Feedbacks in the Historical Period P. Salvi et al. 10.1029/2023JD038984
318. The Land Use Model Intercomparison Project (LUMIP) contribution to CMIP6: rationale and experimental design D. Lawrence et al. 10.5194/gmd-9-2973-2016
319. The Model Intercomparison Project on the climatic response to Volcanic forcing (VolMIP): experimental design and forcing input data for CMIP6 D. Zanchettin et al. 10.5194/gmd-9-2701-2016
320. The reversal of surface wind speed trend in Northeast China: impact from aerosol emissions H. Miao et al. 10.1007/s00382-024-07544-0
321. The Radiative Forcing Model Intercomparison Project (RFMIP): experimental protocol for CMIP6 R. Pincus et al. 10.5194/gmd-9-3447-2016
322. C4MIP – The Coupled Climate–Carbon Cycle Model Intercomparison Project: experimental protocol for CMIP6 C. Jones et al. 10.5194/gmd-9-2853-2016