183 citations as recorded by crossref.

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6. Emergent constraints on equilibrium climate sensitivity in CMIP5: do they hold for CMIP6? M. Schlund et al. 10.5194/esd-11-1233-2020
7. Scale‐Aware and Definition‐Aware Evaluation of Modeled Near‐Surface Precipitation Frequency Using CloudSat Observations J. Kay et al. 10.1002/2017JD028213
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9. Opinion: The scientific and community-building roles of the Geoengineering Model Intercomparison Project (GeoMIP) – past, present, and future D. Visioni et al. 10.5194/acp-23-5149-2023
10. Changes in floodplain regimes over Canada due to climate change impacts: Observations from CMIP6 models M. Mohanty & S. Simonovic 10.1016/j.scitotenv.2021.148323
11. Feedback mechanisms of shallow convective clouds in a warmer climate as demonstrated by changes in buoyancy G. Dagan et al. 10.1088/1748-9326/aac178
12. Ice and mixed-phase cloud statistics on the Antarctic Plateau W. Cossich et al. 10.5194/acp-21-13811-2021
13. Plant Physiology Increases the Magnitude and Spread of the Transient Climate Response to CO2 in CMIP6 Earth System Models C. Zarakas et al. 10.1175/JCLI-D-20-0078.1
14. Evaluation of cloud and precipitation processes in regional and global models with ULTIMATE (ULTra-sIte for Measuring Atmosphere of Tokyo metropolitan Environment): a case study using the dual-polarization Doppler weather radars M. Satoh et al. 10.1186/s40645-022-00511-5
15. Seasonal and interannual characteristics of atmospheric cloud radiative effect over South China and neighbouring ocean regions J. Li et al. 10.1002/joc.8271
16. Evaluation of Southern Ocean cloud in the HadGEM3 general circulation model and MERRA-2 reanalysis using ship-based observations P. Kuma et al. 10.5194/acp-20-6607-2020
17. Climate Change Feedbacks in Aquaplanet Experiments With Explicit and Parametrized Convection for Horizontal Resolutions of 2,525 Up to 5 km M. Retsch et al. 10.1029/2019MS001677
18. Estimated cloud-top entrainment index explains positive low-cloud-cover feedback T. Koshiro et al. 10.1073/pnas.2200635119
19. The Cloud_cci simulator v1.0 for the Cloud_cci climate data record and its application to a global and a regional climate model S. Eliasson et al. 10.5194/gmd-12-829-2019
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21. The Atmospheric Pathway of the Cloud-Radiative Impact on the Circulation Response to Global Warming: Important and Uncertain A. Voigt et al. 10.1175/JCLI-D-18-0810.1
22. Assessment of the Southern Ocean Sea Surface Temperature Biases in CMIP5 and CMIP6 Models Z. Gao et al. 10.1007/s11802-024-5808-5
23. Changes in clouds and thermodynamics under solar geoengineering and implications for required solar reduction R. Russotto & T. Ackerman 10.5194/acp-18-11905-2018
24. Attributing Historical and Future Evolution of Radiative Feedbacks to Regional Warming Patterns using a Green’s Function Approach: The Preeminence of the Western Pacific Y. Dong et al. 10.1175/JCLI-D-18-0843.1
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26. Temporal and Spatial Characteristics of Short-Term Cloud Feedback on Global and Local Interannual Climate Fluctuations from A-Train Observations Q. Yue et al. 10.1175/JCLI-D-18-0335.1
27. Robustness and drivers of the Northern Hemisphere extratropical atmospheric circulation response to a CO$$_2$$-induced warming in CNRM-CM6-1 T. Oudar et al. 10.1007/s00382-019-05113-4
28. Impact of ITCZ width on global climate: ITCZ-MIP A. Pendergrass et al. 10.5194/gmd-17-6365-2024
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31. 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
32. Diurnally asymmetric cloud cover trends amplify greenhouse warming H. Luo et al. 10.1126/sciadv.ado5179
33. 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
34. Does Disabling Cloud Radiative Feedbacks Change Spatial Patterns of Surface Greenhouse Warming and Cooling? J. Chalmers et al. 10.1175/JCLI-D-21-0391.1
35. Asymmetric Cloud‐Shortwave Radiation‐Sea Surface Temperature Feedback of Ningaloo Niño/Niña T. Tozuka & P. Oettli 10.1029/2018GL079869
36. Incorporation of inline warm rain diagnostics into the COSP2 satellite simulator for process-oriented model evaluation T. Michibata et al. 10.5194/gmd-12-4297-2019
37. Evaluating Climate Models’ Cloud Feedbacks Against Expert Judgment M. Zelinka et al. 10.1029/2021JD035198
38. Robust changes in global subtropical circulation under greenhouse warming S. Zhou et al. 10.1038/s41467-023-44244-5
39. Negligible Unforced Historical Pattern Effect on Climate Feedback Strength Found in HadISST-Based AMIP Simulations N. Lewis & T. Mauritsen 10.1175/JCLI-D-19-0941.1
40. Changing Characteristics of Tropical Extreme Precipitation–Cloud Regimes in Warmer Climates W. Lau et al. 10.3390/atmos14060995
41. The Dependence of Global Cloud and Lapse Rate Feedbacks on the Spatial Structure of Tropical Pacific Warming T. Andrews & M. Webb 10.1175/JCLI-D-17-0087.1
42. Marine Low Clouds and their Parameterization in Climate Models H. KAWAI & S. SHIGE 10.2151/jmsj.2020-059
43. Clouds and Convective Self‐Aggregation in a Multimodel Ensemble of Radiative‐Convective Equilibrium Simulations A. Wing et al. 10.1029/2020MS002138
44. Benchmark Calculations of Radiative Forcing by Greenhouse Gases R. Pincus et al. 10.1029/2020JD033483
45. An evaluation of the Arctic clouds and surface radiative fluxes in CMIP6 models J. Wei et al. 10.1007/s13131-021-1705-6
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47. The climate response to increased cloud liquid water over the Arctic in CESM1: a sensitivity study of Wegener–Bergeron–Findeisen process Y. Huang et al. 10.1007/s00382-021-05648-5
48. Investigating Parametric Dependence of Climate Feedbacks in the Atmospheric Component of CNRM‐CM6‐1 S. Peatier et al. 10.1029/2021GL095084
49. Estimating the Effective Radiative Forcing of Contrail Cirrus M. Bickel et al. 10.1175/JCLI-D-19-0467.1
50. Global Land Monsoon Precipitation Changes in CMIP6 Projections Z. Chen et al. 10.1029/2019GL086902
51. Causes of the weak emergent constraint on climate sensitivity at the Last Glacial Maximum M. Renoult et al. 10.5194/cp-19-323-2023
52. Climate Models Underestimate Dynamic Cloud Feedbacks in the Tropics P. Hill et al. 10.1029/2023GL104573
53. Comparison of Coupled Model Intercomparison Project Phases 5 and 6 in Simulating Diurnal Cloud Cycle Z. Jiang et al. 10.3390/atmos15030381
54. Thermodynamic Control on the Poleward Shift of the Extratropical Jet in Climate Change Simulations: The Role of Rising High Clouds and Their Radiative Effects Y. Li et al. 10.1175/JCLI-D-18-0417.1
55. Drier North American Monsoon in Contrast to Asian–African Monsoon under Global Warming C. He et al. 10.1175/JCLI-D-20-0189.1
56. Biased Estimates of Equilibrium Climate Sensitivity and Transient Climate Response Derived From Historical CMIP6 Simulations Y. Dong et al. 10.1029/2021GL095778
57. The utility of simulated ocean chlorophyll observations: a case study with the Chlorophyll Observation Simulator Package (version 1) in CESMv2.2 G. Clow et al. 10.5194/gmd-17-975-2024
58. The Influence of Atmospheric Cloud Radiative Effects on the Large-Scale Stratospheric Circulation Y. Li et al. 10.1175/JCLI-D-16-0643.1
59. Advanced cyberinfrastructure for intercomparison and validation of climate models Z. Sun et al. 10.1016/j.envsoft.2019.104559
60. Fast adjustment versus slow SST-mediated response of daily precipitation statistics to abrupt 4xCO2 H. Douville & A. John 10.1007/s00382-020-05522-w
61. What Are the Main Causes of Positive Subtropical Low Cloud Feedbacks in Climate Models? M. Webb et al. 10.1029/2023MS003716
62. Effectiveness and limitations of parameter tuning in reducing biases of top-of-atmosphere radiation and clouds in MIROC version 5 T. Ogura et al. 10.5194/gmd-10-4647-2017
63. The Diversity of Cloud Responses to Twentieth Century Sea Surface Temperatures L. Silvers et al. 10.1002/2017GL075583
64. Tropospheric Expansion Under Global Warming Reduces Tropical Lower Stratospheric Ozone A. Match & E. Gerber 10.1029/2022GL099463
65. Understanding changes in cloud simulations from E3SM version 1 to version 2 Y. Zhang et al. 10.5194/gmd-17-169-2024
66. Future changes in the wintertime ENSO-NAO teleconnection under greenhouse warming X. Geng et al. 10.1038/s41612-024-00627-z
67. Significant improvement of cloud representation in the global climate model MRI-ESM2 H. Kawai et al. 10.5194/gmd-12-2875-2019
68. A Method for Retrieving Cloud Microphysical Properties Using Combined Measurement of Millimeter-Wave Radar and Lidar W. Lin et al. 10.3390/rs16030586
69. 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
70. Addressing Complexity in Global Aerosol Climate Model Cloud Microphysics U. Proske et al. 10.1029/2022MS003571
71. The Cloud Feedback Model Intercomparison Project Observational Simulator Package: Version 2 D. Swales et al. 10.5194/gmd-11-77-2018
72. On the Correspondence Between Atmosphere‐Only and Coupled Simulations for Radiative Feedbacks and Forcing From CO2 Y. Qin et al. 10.1029/2021JD035460
73. Seasonally and Regionally Dependent Shifts of the Atmospheric Westerly Jets under Global Warming W. Zhou et al. 10.1175/JCLI-D-21-0723.1
74. Robustness of the relationship between tropical high-cloud cover and large-scale circulations A. Noda et al. 10.1007/s00382-024-07441-6
75. Continuous Structural Parameterization: A Proposed Method for Representing Different Model Parameterizations Within One Structure Demonstrated for Atmospheric Convection F. Lambert et al. 10.1029/2020MS002085
76. Changes in Unevenness of Wet‐Day Precipitation Over China During 1961–2020 J. Han et al. 10.1029/2020JD034483
77. Contributions to Polar Amplification in CMIP5 and CMIP6 Models L. Hahn et al. 10.3389/feart.2021.710036
78. A statistical and process-oriented evaluation of cloud radiative effects in high-resolution global models M. Thomas et al. 10.5194/gmd-12-1679-2019
79. The Relationship Between the Present‐Day Seasonal Cycles of Clouds in the Mid‐Latitudes and Cloud‐Radiative Feedback K. Furtado et al. 10.1029/2023GL103902
80. No Cookie for Climate Change A. Voigt & N. Albern 10.1029/2019GL084987
81. Quantifying the Influence of Cloud Radiative Feedbacks on Arctic Surface Warming Using Cloud Locking in an Earth System Model E. Middlemas et al. 10.1029/2020GL089207
82. The Met Office Global Coupled Model 3.0 and 3.1 (GC3.0 and GC3.1) Configurations K. Williams et al. 10.1002/2017MS001115
83. The Potential of a Multidecade Spaceborne Lidar Record to Constrain Cloud Feedback H. Chepfer et al. 10.1002/2017JD027742
84. Hadley cell expansion in CMIP6 models K. Grise & S. Davis 10.5194/acp-20-5249-2020
85. Evaluating Cloud Feedback Components in Observations and Their Representation in Climate Models L. Chao et al. 10.1029/2023JD039427
86. Decoupling of Arctic variability from the North Pacific in a warmer climate S. Jahfer et al. 10.1038/s41612-023-00480-6
87. Model spread and progress in climate modelling J. Jebeile & A. Barberousse 10.1007/s13194-021-00387-0
88. Drivers of the enhanced decline of land near-surface relative humidity to abrupt 4xCO2 in CNRM-CM6-1 H. Douville et al. 10.1007/s00382-020-05351-x
89. The Cloud Feedback Model Intercomparison Project (CFMIP) Diagnostic Codes Catalogue – metrics, diagnostics and methodologies to evaluate, understand and improve the representation of clouds and cloud feedbacks in climate models Y. Tsushima et al. 10.5194/gmd-10-4285-2017
90. The representation of dry-season low-level clouds over Western Equatorial Africa in reanalyses and historical CMIP6 simulations P. Camberlin et al. 10.1007/s00382-023-06714-w
91. A Framework for Stormwater Quality Modelling under the Effects of Climate Change to Enhance Reuse B. Wijesiri et al. 10.3390/su122410463
92. Changes in ENSO-driven Hadley circulation variability under global warming X. Xie et al. 10.1016/j.atmosres.2022.106220
93. Diagnosing Changes of Winter NAO in Response to Different Climate Forcings in a Set of Atmosphere-Only Timeslice Experiments Y. Huang et al. 10.3390/atmos9010010
94. Cloud feedback mechanisms and their representation in global climate models P. Ceppi et al. 10.1002/wcc.465
95. Cloud Response to Arctic Sea Ice Loss and Implications for Future Feedback in the CESM1 Climate Model A. Morrison et al. 10.1029/2018JD029142
96. Using Radar Data to Calibrate a Stochastic Parametrization of Organized Convection E. Cardoso‐Bihlo et al. 10.1029/2018MS001537
97. How accurately can the climate sensitivity to $$\hbox {CO}_{2}$$ be estimated from historical climate change? J. Gregory et al. 10.1007/s00382-019-04991-y
98. Time‐Evolving Radiative Feedbacks in the Historical Period P. Salvi et al. 10.1029/2023JD038984
99. Relative roles of surface temperature and climate forcing patterns in the inconstancy of radiative feedbacks A. Haugstad et al. 10.1002/2017GL074372
100. Ground-based lidar processing and simulator framework for comparing models and observations (ALCF 1.0) P. Kuma et al. 10.5194/gmd-14-43-2021
101. Top‐of‐Atmosphere Radiation Budget and Cloud Radiative Effects Over the Tibetan Plateau and Adjacent Monsoon Regions From CMIP6 Simulations J. Li et al. 10.1029/2020JD034345
102. Application of the Pseudo‐Global Warming Approach in a Kilometer‐Resolution Climate Simulation of the Tropics C. Heim et al. 10.1029/2022JD037958
103. Projection of High Clouds and the Link to Ice Hydrometeors: An Approach Using Long-Term Global Cloud System–Resolving Simulations Y. Chen et al. 10.1175/JCLI-D-21-0150.1
104. Upper Bounds of Maximum Land Surface Temperatures in a Warming Climate and Limits to Plant Growth M. Aminzadeh et al. 10.1029/2023EF003755
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106. Sensitivity of Climate Feedbacks to Vertical Resolution in a General Circulation Model W. Ingram & A. Bushell 10.1029/2020GL092268
107. Impact of Holuhraun volcano aerosols on clouds in cloud-system-resolving simulations M. Haghighatnasab et al. 10.5194/acp-22-8457-2022
108. The influence of direct radiative forcing versus indirect sea surface temperature warming on southern hemisphere subtropical anticyclones under global warming A. Fahad & N. Burls 10.1007/s00382-021-06006-1
109. Investigating the impact of cloud-radiative feedbacks on tropical precipitation extremes B. Medeiros et al. 10.1038/s41612-021-00174-x
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115. Underestimated Passive Volcanic Sulfur Degassing Implies Overestimated Anthropogenic Aerosol Forcing U. Jongebloed et al. 10.1029/2022GL102061
116. Evaluation of aerosol and cloud properties in three climate models using MODIS observations and its corresponding COSP simulator, as well as their application in aerosol–cloud interactions G. Saponaro et al. 10.5194/acp-20-1607-2020
117. Precipitation and the Associated Moist Static Energy Budget off Western Australia in Conjunction with Ningaloo Niño T. Zheng et al. 10.3389/feart.2020.597915
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122. Sensitivities of Simulated Satellite Views of Clouds to Subgrid‐Scale Overlap and Condensate Heterogeneity B. Hillman et al. 10.1029/2017JD027680
123. Evaluation of the CAM6 Climate Model Using Cloud Observations at McMurdo Station, Antarctica J. Yip et al. 10.1029/2021JD034653
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126. Assessment of FY-4A and Himawari-8 Cloud Top Height Retrieval through Comparison with Ground-Based Millimeter Radar at Sites in Tibet and Beijing B. Liu et al. 10.1007/s00376-021-0337-2
127. Analysis of the global atmospheric background sulfur budget in a multi-model framework C. Brodowsky et al. 10.5194/acp-24-5513-2024
128. Clearing clouds of uncertainty M. Zelinka et al. 10.1038/nclimate3402
129. Explicitly Resolved Cloud Feedbacks in the Radiative‐Convective Equilibrium Model Intercomparison Project C. Stauffer & A. Wing 10.1029/2023MS003738
130. Double and Single ITCZs with and without Clouds M. Popp & L. Silvers 10.1175/JCLI-D-17-0062.1
131. Strong Dependence of Atmospheric Feedbacks on Mixed‐Phase Microphysics and Aerosol‐Cloud Interactions in HadGEM3 A. Bodas‐Salcedo et al. 10.1029/2019MS001688
132. Fast‐Forward to Perturbed Equilibrium Climate D. Saint‐Martin et al. 10.1029/2019GL083031
133. Developing a climatological simplification of aerosols to enter the cloud microphysics of a global climate model U. Proske et al. 10.5194/acp-24-5907-2024
134. Observations for Model Intercomparison Project (Obs4MIPs): status for CMIP6 D. Waliser et al. 10.5194/gmd-13-2945-2020
135. Forced summer stationary waves: the opposing effects of direct radiative forcing and sea surface warming H. Baker et al. 10.1007/s00382-019-04786-1
136. Arctic clouds in ECHAM6 and their sensitivity to cloud microphysics and surface fluxes J. Kretzschmar et al. 10.5194/acp-19-10571-2019
137. Diffuse Radiation Forcing Constraints on Gross Primary Productivity and Global Terrestrial Evapotranspiration T. Chakraborty et al. 10.1029/2022EF002805
138. Monsoons, ITCZs, and the Concept of the Global Monsoon R. Geen et al. 10.1029/2020RG000700
139. Diagnosing uncertainties in global biomass burning emission inventories and their impact on modeled air pollutants W. Hua et al. 10.5194/acp-24-6787-2024
140. Historical Simulations With HadGEM3‐GC3.1 for CMIP6 M. Andrews et al. 10.1029/2019MS001995
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144. Updated observations of clouds by MODIS for global model assessment R. Pincus et al. 10.5194/essd-15-2483-2023
145. Forcings, Feedbacks, and Climate Sensitivity in HadGEM3‐GC3.1 and UKESM1 T. Andrews et al. 10.1029/2019MS001866
146. Cloud Feedbacks from CanESM2 to CanESM5.0 and their influence on climate sensitivity J. Virgin et al. 10.5194/gmd-14-5355-2021
147. Causes of Reduced Climate Sensitivity in E3SM From Version 1 to Version 2 Y. Qin et al. 10.1029/2023MS003875
148. Transient and Quasi‐Equilibrium Climate States at 1.5°C and 2°C Global Warming A. King et al. 10.1029/2021EF002274
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152. The fast response of Sahel precipitation to climate change allows effective mitigation action P. Monerie et al. 10.1038/s41612-021-00179-6
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154. State dependence of CO 2 forcing and its implications for climate sensitivity H. He et al. 10.1126/science.abq6872
155. Characteristics analysis of drought at multiple spatiotemporal scale and assessment of CMIP6 performance over the Huaihe River Basin X. Li et al. 10.1016/j.ejrh.2022.101103
156. Revisiting mechanisms of the Mesoamerican Midsummer drought J. García-Franco et al. 10.1007/s00382-022-06338-6
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158. An underestimated negative cloud feedback from cloud lifetime changes J. Mülmenstädt et al. 10.1038/s41558-021-01038-1
159. Overcoming the disconnect between energy system and climate modeling M. Craig et al. 10.1016/j.joule.2022.05.010
160. 21st Century Scenario Forcing Increases More for CMIP6 Than CMIP5 Models H. Fredriksen et al. 10.1029/2023GL102916
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162. Strong cloud–circulation coupling explains weak trade cumulus feedback R. Vogel et al. 10.1038/s41586-022-05364-y
163. Changes in the tropical upper-tropospheric zonal momentum balance due to global warming A. Thakur & J. Sukhatme 10.5194/wcd-5-839-2024
164. The CMIP6 Data Request (DREQ, version 01.00.31) M. Juckes et al. 10.5194/gmd-13-201-2020
165. Diagnosing Transient Response to CO2 Forcing in Coupled Atmosphere‐Ocean Model Experiments Using a Climate Model Emulator J. Tsutsui 10.1029/2019GL085844
166. Understanding Rapid Adjustments to Diverse Forcing Agents C. Smith et al. 10.1029/2018GL079826
167. Southern Ocean cloud and shortwave radiation biases in a nudged climate model simulation: does the model ever get it right? S. Fiddes et al. 10.5194/acp-22-14603-2022
168. Clear-sky control of anvils in response to increased CO2 or surface warming or volcanic eruptions M. Saint-Lu et al. 10.1038/s41612-022-00304-z
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171. An overview of cloud–radiation denial experiments for the Energy Exascale Earth System Model version 1 B. Harrop et al. 10.5194/gmd-17-3111-2024
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