67 citations as recorded by crossref.

1. Analysing the PMIP4-CMIP6 collection: a workflow and tool (pmip_p2fvar_analyzer v1) A. Zhao et al. 10.5194/gmd-15-2475-2022
2. Can southern Australian rainfall decline be explained? A review of possible drivers R. McKay et al. 10.1002/wcc.820
3. The strength, position, and width changes of the intertropical convergence zone since the Last Glacial Maximum S. Yuan et al. 10.1073/pnas.2217064120
4. How certain are El Niño–Southern Oscillation frequency changes in Coupled Model Intercomparison Project Phase 6 models? F. Fix et al. 10.1002/joc.7901
5. AMOC and Climate Responses to Dust Reduction and Greening of the Sahara during the Mid-Holocene M. Zhang et al. 10.1175/JCLI-D-20-0628.1
6. Unraveling forced responses of extreme El Niño variability over the Holocene A. Lawman et al. 10.1126/sciadv.abm4313
7. Evaluation of Dynamical Seasonal Prediction Skills for Tropical Cyclone Activity over the South China Sea in FGOALS-f2 J. Li et al. 10.3390/atmos14010085
8. NUIST ESM v3 Data Submission to CMIP6 J. Cao et al. 10.1007/s00376-020-0173-9
9. Current and Future Climate Extremes Over Latin America and Caribbean: Assessing Earth System Models from High Resolution Model Intercomparison Project (HighResMIP) A. Avila-Diaz et al. 10.1007/s41748-022-00337-7
10. Expansion of winter ENSO‐associated rainfall affected area in Southeast Asia under warmer climate M. Leong et al. 10.1002/joc.8358
11. Future precipitation changes in California: Comparison of CMIP5 and CMIP6 intermodel spread and its drivers D. Petrova et al. 10.1002/joc.8449
12. Evaluating Climate Models with the CLIVAR 2020 ENSO Metrics Package Y. Planton et al. 10.1175/BAMS-D-19-0337.1
13. Different Methods in Assessing El Niño Flavors Lead to Opposite Results I. Abdelkader Di Carlo et al. 10.1029/2023GL104558
14. Global terrestrial monsoon area variations since Last Glacial Maximum based on TraCE21ka and PMIP4-CMIP6 simulations J. Wang et al. 10.1016/j.gloplacha.2023.104308
15. Persistently active El Niño–Southern Oscillation since the Mesozoic X. Li et al. 10.1073/pnas.2404758121
16. Amplitude, duration, variability, and seasonal frequency analysis of the El Niño-Southern Oscillation O. Alizadeh 10.1007/s10584-022-03440-w
17. Speleothem records of monsoon interannual-interdecadal variability through the Holocene S. Parker et al. 10.1088/2515-7620/ac3eaa
18. Strength of the North African monsoon in the Last Interglacial and under future warming J. He et al. 10.1016/j.aosl.2022.100320
19. Future changes in boreal winter ENSO teleconnections in a large ensemble of high-resolution climate simulations N. Johnson et al. 10.3389/fclim.2022.941055
20. Assessing Future Projections of Warm‐Season Marine Heatwave Characteristics With Three CMIP6 Models X. Li & S. Donner 10.1029/2022JC019253
21. Changing El Niño–Southern Oscillation in a warming climate W. Cai et al. 10.1038/s43017-021-00199-z
22. Variability and extremes: statistical validation of the Alfred Wegener Institute Earth System Model (AWI-ESM) J. Contzen et al. 10.5194/gmd-15-1803-2022
23. Coral Oxygen Isotopic Records Capture the 2015/2016 El Niño Event in the Central Equatorial Pacific G. O’Connor et al. 10.1029/2021GL094036
24. The DOE E3SM Model Version 2: Overview of the Physical Model and Initial Model Evaluation J. Golaz et al. 10.1029/2022MS003156
25. The variations of ENSO teleconnections during the Last Interglacial based on PMIP4 simulations J. Ma et al. 10.1016/j.palaeo.2024.112193
26. Spatiotemporal networks for ENSO forecasting with LICOM3 and remote sensing data X. Zhang et al. 10.1016/j.engappai.2023.106641
27. Evolution of the Internal Climate Modes under Future Warming J. Coburn & S. Pryor 10.1175/JCLI-D-22-0200.1
28. Assessment of 21st Century Changing Sea Surface Temperature, Rainfall, and Sea Surface Height Patterns in the Tropical Pacific Islands Using CMIP6 Greenhouse Warming Projections L. Dhage & M. Widlansky 10.1029/2021EF002524
29. The Tropical Pacific Annual Cycle and ENSO in PMIP4 Simulations of the Mid‐Holocene X. Zhang et al. 10.1029/2021JC017587
30. Land–sea temperature contrasts at the Last Interglacial and their impact on the hydrological cycle N. Yeung et al. 10.5194/cp-17-869-2021
31. Seasonal aridity in the Indo-Pacific Warm Pool during the Late Glacial driven by El Niño-like conditions P. Hällberg et al. 10.5194/cp-18-1655-2022
32. A fully calibrated and updated mid-Holocene climate reconstruction for Eastern South America I. Gorenstein et al. 10.1016/j.quascirev.2022.107646
33. Changes in ENSO Characteristics in Model Simulations with Considerably Altered Background Climate States T. Siuts et al. 10.1175/JCLI-D-21-1004.1
34. Future increase in extreme El Niño supported by past glacial changes K. Thirumalai et al. 10.1038/s41586-024-07984-y
35. Indian Ocean variability changes in the Paleoclimate Modelling Intercomparison Project C. Brierley et al. 10.5194/cp-19-681-2023
36. Indian Ocean Dipole Changes During the Last Interglacial Modulated by the Mean Oceanic Climatology S. Liu et al. 10.1029/2023GL106153
37. Relative Contribution of Atmospheric Drivers to “Extreme” Snowfall Over the Amundsen Sea Embayment S. Swetha Chittella et al. 10.1029/2022GL098661
38. High-resolution marine data and transient simulations support orbital forcing of ENSO amplitude since the mid-Holocene M. Carré et al. 10.1016/j.quascirev.2021.107125
39. Large-scale emergence of regional changes in year-to-year temperature variability by the end of the 21st century D. Olonscheck et al. 10.1038/s41467-021-27515-x
40. A review of the El Niño-Southern Oscillation in future O. Alizadeh 10.1016/j.earscirev.2022.104246
41. Phase-Locking of El Niño and La Niña Events in CMIP6 Models Y. Yan & D. Sun 10.3390/atmos15080882
42. A new understanding of the causes of future change in El Niño teleconnection H. Lee & E. Jin 10.1016/j.atmosres.2024.107508
43. Future Weakening of the ENSO Ocean Carbon Buffer Under Anthropogenic Forcing E. Liao et al. 10.1029/2021GL094021
44. Relationships between the Hadley circulation and tropical sea surface temperature with different meridional structures simulated in CMIP6 models Y. Li et al. 10.3389/fmars.2023.1145509
45. ENSO Diversity and the Simulation of Its Teleconnections to Winter Precipitation Extremes Over the US in High Resolution Earth System Models S. Mahajan et al. 10.1029/2022GL102657
46. Reduced El Niño variability in the mid-Pliocene according to the PlioMIP2 ensemble A. Oldeman et al. 10.5194/cp-17-2427-2021
47. Why could ENSO directly affect the occurrence frequency of Arctic daily warming events after the late 1970s? C. Wang et al. 10.1088/1748-9326/acb06f
48. Russian Climate Research in 2019–2022 I. Mokhov 10.1134/S0001433823150100
49. ENSO sentinels in the Americas' humid tropics: We need combined hydrometric and isotopic monitoring for improved El Niño and La Niña impact prediction R. Sánchez‐Murillo et al. 10.1002/hyp.15027
50. Impact of paleoclimate on present and future evolution of the Greenland Ice Sheet H. Yang et al. 10.1371/journal.pone.0259816
51. Performance of the Taiwan Earth System Model in Simulating Climate Variability Compared With Observations and CMIP6 Model Simulations Y. Wang et al. 10.1029/2020MS002353
52. Global El Niño–Southern Oscillation Teleconnections in CMIP6 Models I. Serykh & D. Sonechkin 10.3390/atmos15040500
53. Internal Climate Variability in the Present Climate and the Change in ENSO Amplitude in Future Climate Simulations S. Hyun et al. 10.3389/fclim.2022.932978
54. Selecting CMIP6 GCMs for CORDEX Dynamical Downscaling: Model Performance, Independence, and Climate Change Signals G. Di Virgilio et al. 10.1029/2021EF002625
55. Responses of Tropical Background State and ENSO Behaviors to Mid-Holocene Forcing Simulated by PMIP3 and PMIP4 Models M. Song & L. Chen 10.3389/feart.2022.853577
56. Last Glacial Maximum climate and atmospheric circulation over the Australian region from climate models Y. Du et al. 10.5194/cp-20-393-2024
57. Humidification of Central Asia and equatorward shifts of westerly winds since the late Pliocene Y. Zhong et al. 10.1038/s43247-022-00604-5
58. Projected ENSO teleconnection on the Southeast Asian climate under global warming D. Nguyen–Le 10.1088/1748-9326/ad0d3e
59. ENSO-driven extreme oscillations in mean sea level destabilise critical shoreline mangroves—An emerging threat N. Duke et al. 10.1371/journal.pclm.0000037
60. A Potential Reason for a More CP El Nino‐Like SSTA Performance in CMIP6 Simulations L. Wang & Y. Lin 10.1029/2023GL105092
61. Russian Climate Research in 2019–2022 I. Mokhov 10.31857/S0002351523070106
62. Towards understanding the robust strengthening of ENSO and more frequent extreme El Niño events in CMIP6 global warming simulations U. Heede & A. Fedorov 10.1007/s00382-023-06856-x
63. Evidence of anthropogenic impacts on global drought frequency, duration, and intensity F. Chiang et al. 10.1038/s41467-021-22314-w
64. Dynamics for El Niño-La Niña asymmetry constrain equatorial-Pacific warming pattern M. Hayashi et al. 10.1038/s41467-020-17983-y
65. Variability of surface climate in simulations of past and future K. Rehfeld et al. 10.5194/esd-11-447-2020
66. Large-scale features and evaluation of the PMIP4-CMIP6 <i>midHolocene</i> simulations C. Brierley et al. 10.5194/cp-16-1847-2020
67. Uncertainty of ENSO-amplitude projections in CMIP5 and CMIP6 models G. Beobide-Arsuaga et al. 10.1007/s00382-021-05673-4