96 citations as recorded by crossref.

1. Projections of the Transient State‐Dependency of Climate Feedbacks R. Bastiaansen et al. 10.1029/2021GL094670
2. Cloud and Surface Albedo Feedbacks Reshape 21st Century Warming in Successive Generations of An Earth System Model D. Schneider et al. 10.1029/2022GL100653
3. CO<sub>2</sub>-equivalence metrics for surface albedo change based on the radiative forcing concept: a critical review R. Bright & M. Lund 10.5194/acp-21-9887-2021
4. Joint optimization of land carbon uptake and albedo can help achieve moderate instantaneous and long-term cooling effects A. Graf et al. 10.1038/s43247-023-00958-4
5. Contrasting fast and slow intertropical convergence zone migrations linked to delayed Southern Ocean warming W. Liu et al. 10.1038/s41558-024-02034-x
6. Evaluating the Nature and Extent of Changes to Climate Sensitivity Between FGOALS‐g2 and FGOALS‐g3 H. Wang et al. 10.1029/2021JD035852
7. The Emergence and Transient Nature of Arctic Amplification in Coupled Climate Models M. Holland & L. Landrum 10.3389/feart.2021.719024
8. The Effect of Atmospheric Transmissivity on Model and Observational Estimates of the Sea Ice Albedo Feedback A. Donohoe et al. 10.1175/JCLI-D-19-0674.1
9. High Climate Sensitivity in the Community Earth System Model Version 2 (CESM2) A. Gettelman et al. 10.1029/2019GL083978
10. Historical total ozone radiative forcing derived from CMIP6 simulations R. Skeie et al. 10.1038/s41612-020-00131-0
11. Arctic climate feedback response to local sea-ice concentration and remote sea surface temperature changes in PAMIP simulations M. Jenkins et al. 10.1007/s00382-024-07465-y
12. Reduced terrestrial evaporation increases atmospheric water vapor by generating cloud feedbacks M. Laguë et al. 10.1088/1748-9326/acdbe1
13. Climate impact of surface albedo change in Life Cycle Assessment: Implications of site and time dependence P. Sieber et al. 10.1016/j.eiar.2019.04.003
14. Climate Sensitivity is Sensitive to Changes in Ocean Heat Transport H. Singh et al. 10.1175/JCLI-D-21-0674.1
15. Shutdown of Southern Ocean convection controls long-term greenhouse gas-induced warming A. Gjermundsen et al. 10.1038/s41561-021-00825-x
16. A Semi‐Analytical Model for Water Vapor, Temperature, and Surface‐Albedo Feedbacks in Comprehensive Climate Models N. Feldl & T. Merlis 10.1029/2023GL105796
17. Cloud Response to Arctic Sea Ice Loss and Implications for Future Feedback in the CESM1 Climate Model A. Morrison et al. 10.1029/2018JD029142
18. New Estimates of Aerosol Direct Radiative Effects and Forcing From A‐Train Satellite Observations A. Matus et al. 10.1029/2019GL083656
19. Accounting for albedo change to identify climate-positive tree cover restoration N. Hasler et al. 10.1038/s41467-024-46577-1
20. The Dependence of Mean Climate State on Shortwave Absorption by Water Vapor H. Kim et al. 10.1175/JCLI-D-21-0417.1
21. Advances in Atmospheric Radiation: Theories, Models, and Their Applications. Part II: Radiative Transfer Models and Related Applications H. Zhang et al. 10.1007/s13351-024-3089-y
22. Albedo changes caused by future urbanization contribute to global warming Z. Ouyang et al. 10.1038/s41467-022-31558-z
23. Diagnosing Instantaneous Forcing and Feedbacks of Downwelling Longwave Radiation at the Surface: A Simple Methodology and Its Application to CMIP5 Models C. Shakespeare & M. Roderick 10.1175/JCLI-D-21-0865.1
24. Changes in clouds and thermodynamics under solar geoengineering and implications for required solar reduction R. Russotto & T. Ackerman 10.5194/acp-18-11905-2018
25. Effective radiative forcing and adjustments in CMIP6 models C. Smith et al. 10.5194/acp-20-9591-2020
26. Better calibration of cloud parameterizations and subgrid effects increases the fidelity of the E3SM Atmosphere Model version 1 P. Ma et al. 10.5194/gmd-15-2881-2022
27. Non‐Monotonic Feedback Dependence Under Abrupt CO2 Forcing Due To a North Atlantic Pattern Effect I. Mitevski et al. 10.1029/2023GL103617
28. Exploiting SMILEs and the CMIP5 Archive to Understand Arctic Climate Change Seasonality and Uncertainty Y. Wu et al. 10.1029/2022GL100745
29. Time‐Evolving Radiative Feedbacks in the Historical Period P. Salvi et al. 10.1029/2023JD038984
30. Sea ice feedbacks cause more greenhouse cooling than greenhouse warming at high northern latitudes on multi-century timescales J. Kay et al. 10.1088/2752-5295/ad8026
31. Observation‐Based Radiative Kernels From CloudSat/CALIPSO R. Kramer et al. 10.1029/2018JD029021
32. Causes of Higher Climate Sensitivity in CMIP6 Models M. Zelinka et al. 10.1029/2019GL085782
33. Invariability of Arctic Top‐of‐Atmosphere Radiative Response to Surface Temperature Changes J. Hwang et al. 10.1029/2020EA001316
34. Radiative Effects and Costing Assessment of Arctic Sea Ice Albedo Changes H. Hao et al. 10.3390/rs15040970
35. Impacts of Atlantic meridional overturning circulation weakening on Arctic amplification Y. Lee et al. 10.1073/pnas.2402322121
36. Ultrafast Arctic amplification and its governing mechanisms T. Janoski et al. 10.1088/2752-5295/ace211
37. Arctic Amplification: A Rapid Response to Radiative Forcing M. Previdi et al. 10.1029/2020GL089933
38. The effect of rapid adjustments to halocarbons and N2O on radiative forcing Ø. Hodnebrog et al. 10.1038/s41612-020-00150-x
39. Substantial twentieth-century Arctic warming caused by ozone-depleting substances L. Polvani et al. 10.1038/s41558-019-0677-4
40. The Earth system model CLIMBER-X v1.0 – Part 1: Climate model description and validation​​​​​​​​​​​​​​ M. Willeit et al. 10.5194/gmd-15-5905-2022
41. Developing a monthly radiative kernel for surface albedo change from satellite climatologies of Earth's shortwave radiation budget: CACK v1.0 R. Bright & T. O'Halloran 10.5194/gmd-12-3975-2019
42. Stronger Arctic amplification produced by decreasing, not increasing, CO2 concentrations S. Zhou et al. 10.1088/2752-5295/aceea2
43. Evaluation of Sea Ice Radiative Forcing according to Surface Albedo and Skin Temperature over the Arctic from 1982–2015 N. Seong et al. 10.3390/rs14112512
44. Last Glacial Maximum (LGM) climate forcing and ocean dynamical feedback and their implications for estimating climate sensitivity J. Zhu & C. Poulsen 10.5194/cp-17-253-2021
45. The Dominant Contribution of Southern Ocean Heat Uptake to Time‐Evolving Radiative Feedback in CESM Y. Lin et al. 10.1029/2021GL093302
46. Evaluating Climate Models’ Cloud Feedbacks Against Expert Judgment M. Zelinka et al. 10.1029/2021JD035198
47. Thermodynamic effect dictates influence of the Atlantic Multidecadal Oscillation on Eurasia winter temperature H. Wang et al. 10.1038/s41612-024-00686-2
48. 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
49. Roman Warm Period and Late Antique Little Ice Age in an Earth System Model Large Ensemble F. Shi et al. 10.1029/2021JD035832
50. Quantifying long-term cloud feedback over East Asia combining with radiative kernels and CMIP6 data M. Liu et al. 10.1007/s00382-022-06577-7
51. An Assessment of Short-term Global and East Asian Local Climate Feedbacks using New Radiative Kernels F. Wang et al. 10.1007/s00382-022-06369-z
52. Radiative sensitivity quantified by a new set of radiation flux kernels based on the ECMWF Reanalysis v5 (ERA5) H. Huang & Y. Huang 10.5194/essd-15-3001-2023
53. Forest composition change and biophysical climate feedbacks across boreal North America R. Massey et al. 10.1038/s41558-023-01851-w
54. Net Climate Effects of Moose Browsing in Early Successional Boreal Forests by Integrating Carbon and Albedo Dynamics J. Salisbury et al. 10.1029/2022JG007279
55. Contributions to Polar Amplification in CMIP5 and CMIP6 Models L. Hahn et al. 10.3389/feart.2021.710036
56. Understanding the surface temperature response and its uncertainty to CO<sub>2</sub>, CH<sub>4</sub>, black carbon, and sulfate K. Nordling et al. 10.5194/acp-21-14941-2021
57. Stronger Arctic amplification from ozone-depleting substances than from carbon dioxide Y. Liang et al. 10.1088/1748-9326/ac4a31
58. Water vapor and lapse rate feedbacks in the climate system R. Colman & B. Soden 10.1103/RevModPhys.93.045002
59. Surface warming and wetting due to methane’s long-wave radiative effects muted by short-wave absorption R. Allen et al. 10.1038/s41561-023-01144-z
60. Reponses of Land Surface Albedo to Global Vegetation Greening: An Analysis Using GLASS Data X. Li et al. 10.3390/atmos14010031
61. Evaluating Climate Model Simulations of the Radiative Forcing and Radiative Response at Earth’s Surface R. Kramer et al. 10.1175/JCLI-D-18-0137.1
62. Sea ice and atmospheric circulation shape the high-latitude lapse rate feedback N. Feldl et al. 10.1038/s41612-020-00146-7
63. Arctic Climate Feedbacks in ERA5 Reanalysis: Seasonal and Spatial Variations and the Impact of Sea‐Ice Loss M. Jenkins & A. Dai 10.1029/2022GL099263
64. The radiative feedback continuum from Snowball Earth to an ice-free hothouse I. Eisenman & K. Armour 10.1038/s41467-024-50406-w
65. Assessing Global and Local Radiative Feedbacks Based on AGCM Simulations for 1980–2014/2017 R. Zhang et al. 10.1029/2020GL088063
66. Changes in Poleward Atmospheric Energy Transport over a Wide Range of Climates: Energetic and Diffusive Perspectives and A Priori Theories T. Merlis et al. 10.1175/JCLI-D-21-0682.1
67. Controls of the transient climate response to emissions by physical feedbacks, heat uptake and carbon cycling R. Williams et al. 10.1088/1748-9326/ab97c9
68. Local Radiative Feedbacks Over the Arctic Based on Observed Short‐Term Climate Variations R. Zhang et al. 10.1029/2018GL077852
69. Uncertainty in the Evolution of Climate Feedback Traced to the Strength of the Atlantic Meridional Overturning Circulation Y. Lin et al. 10.1029/2019GL083084
70. Process Drivers, Inter-Model Spread, and the Path Forward: A Review of Amplified Arctic Warming P. Taylor et al. 10.3389/feart.2021.758361
71. Cloud Feedbacks from CanESM2 to CanESM5.0 and their influence on climate sensitivity J. Virgin et al. 10.5194/gmd-14-5355-2021
72. Radiative feedbacks on land surface change and associated tropical precipitation shifts M. Laguë et al. 10.1175/JCLI-D-20-0883.1
73. Removal of Atmospheric Methane by Increasing Hydroxyl Radicals via a Water Vapor Enhancement Strategy Y. Liu et al. 10.3390/atmos15091046
74. Trends and Variability of Atmospheric Downward Longwave Radiation Over China From 1958 to 2015 Y. Wei et al. 10.1029/2020EA001370
75. Quantifying the Cloud Particle‐Size Feedback in an Earth System Model J. Zhu & C. Poulsen 10.1029/2019GL083829
76. A chlorophyll-deficient, highly reflective soybean mutant: radiative forcing and yield gaps L. Genesio et al. 10.1088/1748-9326/ab865e
77. The HadGEM3-GA7.1 radiative kernel: the importance of a well-resolved stratosphere C. Smith et al. 10.5194/essd-12-2157-2020
78. Reconstruction of Historical Land Surface Albedo Changes in China From 850 to 2015 Using Land Use Harmonization Data and Albedo Look‐Up Maps Y. Song et al. 10.1029/2021EA001799
79. Atmospheric Circulation Sensitivity to Changes in the Vertical Structure of Polar Warming D. Kim et al. 10.1029/2021GL094726
80. Last Glacial Maximum pattern effects reduce climate sensitivity estimates V. Cooper et al. 10.1126/sciadv.adk9461
81. Divergent global-scale temperature effects from identical aerosols emitted in different regions G. Persad & K. Caldeira 10.1038/s41467-018-05838-6
82. Drivers of elevation-dependent warming over the Tibetan Plateau S. Hu & P. Hsu 10.1016/j.aosl.2022.100289
83. Observational Evidence of Increasing Global Radiative Forcing R. Kramer et al. 10.1029/2020GL091585
84. Change in Climate Sensitivity and Its Dependence on the Lapse-Rate Feedback in 4 × CO2 Climate Model Experiments K. Eiselt & R. Graversen 10.1175/JCLI-D-21-0623.1
85. Band-by-band spectral radiative kernels based on the ERA5 reanalysis H. Huang et al. 10.1038/s41597-024-03080-y
86. Does Surface Temperature Respond to or Determine Downwelling Longwave Radiation? L. Vargas Zeppetello et al. 10.1029/2019GL082220
87. Oceanic Influence and Lapse Rate Changes Dominate the Recent Amplified Saharan Warming L. Zhuo & B. Rose 10.1029/2023GL106961
88. Asymmetric Warming/Cooling Response to CO2 Increase/Decrease Mainly Due To Non‐Logarithmic Forcing, Not Feedbacks I. Mitevski et al. 10.1029/2021GL097133
89. Evaluation of CloudSat Radiative Kernels Using ARM and CERES Observations and ERA5 Reanalysis N. Dai et al. 10.1029/2020JD034510
90. Relationships among Arctic warming, sea-ice loss, stability, lapse rate feedback, and Arctic amplification A. Dai & M. Jenkins 10.1007/s00382-023-06848-x
91. Effective radiative forcing from emissions of reactive gases and aerosols – a multi-model comparison G. Thornhill et al. 10.5194/acp-21-853-2021
92. The Impact of Sea‐Ice Loss on Arctic Climate Feedbacks and Their Role for Arctic Amplification M. Jenkins & A. Dai 10.1029/2021GL094599
93. Understanding Rapid Adjustments to Diverse Forcing Agents C. Smith et al. 10.1029/2018GL079826
94. Review of Land Surface Albedo: Variance Characteristics, Climate Effect and Management Strategy X. Zhang et al. 10.3390/rs14061382
95. Nonlinear Coupling Between Longwave Radiative Climate Feedbacks H. Huang & Y. Huang 10.1029/2020JD033995
96. A refined model for the Earth’s global energy balance P. Ceppi & J. Gregory 10.1007/s00382-019-04825-x