143 citations as recorded by crossref.

1. Labrador Sea subsurface density as a precursor of multidecadal variability in the North Atlantic: a multi-model study P. Ortega et al. 10.5194/esd-12-419-2021
2. Earth system models for regional environmental management of red tide: Prospects and limitations of current generation models and next generation development A. Elshall et al. 10.1007/s12665-022-10343-7
3. Does Increasing Climate Model Horizontal Resolution Be Beneficial for the Mediterranean Region?: Multimodel Evaluation Framework for High‐Resolution Model Intercomparison Project A. Mishra et al. 10.1029/2022JD037812
4. Partitioning climate uncertainty in ecological projections: Pacific oysters in a hotter Europe R. Wilson et al. 10.1016/j.ecoinf.2024.102537
5. Assessment of NEX-GDDP-CMIP6 Downscale Data in Simulating Extreme Precipitation over the Huai River Basin F. Jiang et al. 10.3390/atmos14101497
6. Impact of resolution on the atmosphere–ocean coupling along the Gulf Stream in global high resolution models E. Tsartsali et al. 10.1007/s00382-021-06098-9
7. The Influence of Ocean Coupling on Simulated and Projected Tropical Cyclone Precipitation in the HighResMIP–PRIMAVERA Simulations H. Huang et al. 10.1029/2021GL094801
8. The Northern Hemisphere Wintertime Storm Track Simulated in the High‐Resolution Community Earth System Model Z. Wang et al. 10.1029/2023MS003652
9. The Atmospheric Response to Meridional Shifts of the Gulf Stream SST Front and Its Dependence on Model Resolution L. Famooss Paolini et al. 10.1175/JCLI-D-21-0530.1
10. Influence of model resolution on bomb cyclones revealed by HighResMIP-PRIMAVERA simulations G. Jiaxiang et al. 10.1088/1748-9326/ab88fa
11. Quantifying Progress Across Different CMIP Phases With the ESMValTool L. Bock et al. 10.1029/2019JD032321
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13. The Evaluation of the North Atlantic Climate System in UKESM1 Historical Simulations for CMIP6 J. Robson et al. 10.1029/2020MS002126
14. The Sensitivity of British Weather to Ocean Tides A. Arnold et al. 10.1029/2020GL090732
15. Global Dust Variability Explained by Drought Sensitivity in CMIP6 Models Y. Aryal & S. Evans 10.1029/2021JF006073
16. Evaluation of Asian summer precipitation in different configurations of a high-resolution general circulation model in a range of decision-relevant spatial scales M. Muetzelfeldt et al. 10.5194/hess-25-6381-2021
17. Sea Ice—Ocean Interactions in the Barents Sea Modeled at Different Resolutions D. Docquier et al. 10.3389/feart.2020.00172
18. Past long-term summer warming over western Europe in new generation climate models: role of large-scale atmospheric circulation J. Boé et al. 10.1088/1748-9326/ab8a89
19. North Atlantic gyre circulation in PRIMAVERA models V. Meccia et al. 10.1007/s00382-021-05686-z
20. Response of convective systems to the orbital forcing of the last interglacial in a global nonhydrostatic atmospheric model with and without a convective parameterization M. Chikira et al. 10.1007/s00382-021-06056-5
21. The double‐ITCZ problem in CMIP6 and the influences of deep convection and model resolution X. Ma et al. 10.1002/joc.7980
22. 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
23. Evaluation of global teleconnections in CMIP6 climate projections using complex networks C. Dalelane et al. 10.5194/esd-14-17-2023
24. An Assessment of Nonhydrostatic and Hydrostatic Dynamical Cores at Seasonal Time Scales in the Energy Exascale Earth System Model (E3SM) W. Liu et al. 10.1029/2021MS002805
25. Increasing Hurricane Intensification Rate Near the US Atlantic Coast K. Balaguru et al. 10.1029/2022GL099793
26. Resolving and Parameterising the Ocean Mesoscale in Earth System Models H. Hewitt et al. 10.1007/s40641-020-00164-w
27. An inter-comparison of the mass budget of the Arctic sea ice in CMIP6 models A. Keen et al. 10.5194/tc-15-951-2021
28. Future Projections of Multiple Tropical Cyclone Events in the Northern Hemisphere in the CMIP6‐HighResMIP Models Z. Fu et al. 10.1029/2023GL103064
29. North Pacific trade wind precursors to ENSO in the CMIP6 HighResMIP multimodel ensemble V. Pivotti et al. 10.1007/s00382-022-06449-0
30. Sensitivity of the Atlantic Meridional Overturning Circulation to Model Resolution in CMIP6 HighResMIP Simulations and Implications for Future Changes M. Roberts et al. 10.1029/2019MS002014
31. Northern Hemisphere blocking simulation in current climate models: evaluating progress from the Climate Model Intercomparison Project Phase 5 to 6 and sensitivity to resolution R. Schiemann et al. 10.5194/wcd-1-277-2020
32. Evaluation of the contribution of tropical cyclone seeds to changes in tropical cyclone frequency due to global warming in high-resolution multi-model ensemble simulations Y. Yamada et al. 10.1186/s40645-020-00397-1
33. Asymmetries in the Southern Ocean contribution to global heat and carbon uptake R. Williams et al. 10.1038/s41558-024-02066-3
34. How well do the CMIP6 HighResMIP models simulate precipitation over the Tibetan Plateau? Q. Chen et al. 10.1016/j.atmosres.2022.106393
35. Effect of Resolving Ocean Eddies on the Transient Response of Global Mean Surface Temperature to Abrupt 4xCO2 Forcing D. Putrasahan et al. 10.1029/2020GL092049
36. Application-specific optimal model weighting of global climate models: A red tide example A. Elshall et al. 10.1016/j.cliser.2022.100334
37. Current and Potential Future Global Distribution of the Raisin Moth Cadra figulilella (Lepidoptera: Pyralidae) under Two Different Climate Change Scenarios B. Wang et al. 10.3390/biology12030435
38. Subpolar Atlantic Ocean mixed layer heat content variability is increasingly driven by an active ocean S. Josey & B. Sinha 10.1038/s43247-022-00433-6
39. Improved representation of plant physiology in the JULES-vn5.6 land surface model: photosynthesis, stomatal conductance and thermal acclimation R. Oliver et al. 10.5194/gmd-15-5567-2022
40. To what extent horizontal resolution improves the simulation of precipitation in CMIP6 HighResMIP models over Southwest China? Z. Jin et al. 10.3389/feart.2022.1003748
41. Mesoscale eddies inhibit intensification of the Subantarctic Front under global warming D. Li et al. 10.1088/1748-9326/ad8173
42. Opinion: Optimizing climate models with process knowledge, resolution, and artificial intelligence T. Schneider et al. 10.5194/acp-24-7041-2024
43. An Unprecedented Set of High‐Resolution Earth System Simulations for Understanding Multiscale Interactions in Climate Variability and Change P. Chang et al. 10.1029/2020MS002298
44. Enhanced Upper Ocean Warming Projected by the Eddy‐Resolving Community Earth System Model G. Xu et al. 10.1029/2023GL106100
45. FORTE 2.0: a fast, parallel and flexible coupled climate model A. Blaker et al. 10.5194/gmd-14-275-2021
46. Role of atmospheric horizontal resolution in simulating tropical and subtropical South American precipitation in HadGEM3-GC31 P. Monerie et al. 10.5194/gmd-13-4749-2020
47. Heat Balance in the Nordic Seas in a Global 1/12° Coupled Model A. Treguier et al. 10.1175/JCLI-D-20-0063.1
48. ENSO phase-locking behavior in climate models: from CMIP5 to CMIP6 M. Liu et al. 10.1088/2515-7620/abf295
49. Remote Versus Local Impacts of Energy Backscatter on the North Atlantic SST Biases in a Global Ocean Model C. Chang et al. 10.1029/2023GL105757
50. Tropical cyclone precipitation in the HighResMIP atmosphere-only experiments of the PRIMAVERA Project W. Zhang et al. 10.1007/s00382-021-05707-x
51. Projected Changes to Wintertime Air‐Sea Turbulent Heat Fluxes Over the Subpolar North Atlantic Ocean C. Barrell et al. 10.1029/2022EF003337
52. The role of the Southern Ocean in the global climate response to carbon emissions R. Williams et al. 10.1098/rsta.2022.0062
53. Projected changes in precipitation and air temperature over the Volga River Basin from bias-corrected CMIP6 outputs S. Hoseini et al. 10.61186/NMCE.2303.1034
54. Air-Sea interaction over the Gulf Stream in an ensemble of HighResMIP present climate simulations A. Bellucci et al. 10.1007/s00382-020-05573-z
55. Mesoscale Convective Systems Simulated by a High‐Resolution Global Nonhydrostatic Model Over the United States and China Y. Na et al. 10.1029/2021JD035916
56. Evaluating surface eddy properties in coupled climate simulations with ‘eddy-present’ and ‘eddy-rich’ ocean resolution S. Moreton et al. 10.1016/j.ocemod.2020.101567
57. Detection and Attribution of Climate Change Using a Neural Network C. Bône et al. 10.1029/2022MS003475
58. Projecting irrigation demand under IPCC climate change scenarios using WEAP modeling in the Rechna Doab, Pakistan H. Khan & Z. Bin Zahid 10.1016/j.clwat.2024.100040
59. Understanding the Sensitivity of the North Atlantic Subpolar Overturning in Different Resolution Versions of HadGEM3‐GC3.1 T. Petit et al. 10.1029/2023JC019672
60. Evaluation of CMIP6 HighResMIP Models and ERA5 Reanalysis in Simulating Summer Precipitation over the Tibetan Plateau T. Chen et al. 10.3390/atmos14061015
61. Delayed Antarctic sea-ice decline in high-resolution climate change simulations T. Rackow et al. 10.1038/s41467-022-28259-y
62. 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
63. The effect of geographic sampling on evaluation of extreme precipitation in high-resolution climate models M. Risser & M. Wehner 10.5194/ascmo-6-115-2020
64. The Relationship Between African Easterly Waves and Tropical Cyclones in Historical and Future Climates in the HighResMIP‐PRIMAVERA Simulations E. Bercos‐Hickey et al. 10.1029/2022JD037471
65. ENSO affects the North Atlantic Oscillation 1 year later A. Scaife et al. 10.1126/science.adk4671
66. The importance of horizontal model resolution on simulated precipitation in Europe – from global to regional models G. Strandberg & P. Lind 10.5194/wcd-2-181-2021
67. The sea ice component of GC5: coupling SI3 to HadGEM3 using conductive fluxes E. Blockley et al. 10.5194/gmd-17-6799-2024
68. On warm bias and mesoscale dynamics setting the Southern Ocean large-scale circulation mean state M. Zeller & T. Martin 10.1016/j.ocemod.2024.102426
69. Extratropical Transition of Tropical Cyclones in a Multiresolution Ensemble of Atmosphere-Only and Fully Coupled Global Climate Models A. Baker et al. 10.1175/JCLI-D-21-0801.1
70. Future Evolution of an Eddy Rich Ocean Associated with Enhanced East Atlantic Storminess in a Coupled Model Projection J. Grist et al. 10.1029/2021GL092719
71. Sensitivity of ECMWF coupled forecasts to improved initialization of the ocean mesoscale C. Roberts et al. 10.1002/qj.4383
72. Climate change/variability and hydrological modelling studies in Zimbabwe: a review of progress and knowledge gaps A. Maviza & F. Ahmed 10.1007/s42452-021-04512-9
73. Greenhouse-gas forced changes in the Atlantic meridional overturning circulation and related worldwide sea-level change M. Couldrey et al. 10.1007/s00382-022-06386-y
74. Investigating the skills of HighResMIP in capturing historical and future mean precipitation shifts over Pakistan K. Eman et al. 10.1002/joc.8558
75. Sea Surface Temperature–Salinity Covariability and Its Scale‐Dependent Characteristics S. Kido et al. 10.1029/2021GL096010
76. Global mapping and evolution of persistent fronts in Large Marine Ecosystems over the past 40 years Q. Xing et al. 10.1038/s41467-024-48566-w
77. Projected future changes in bomb cyclones by the HighResMIP-PRIMAVERA multimodel ensemble J. Gao et al. 10.1007/s00382-024-07327-7
78. The Role of the North Atlantic Oscillation for Projections of Winter Mean Precipitation in Europe C. McKenna & A. Maycock 10.1029/2022GL099083
79. Dust emission response to precipitation and temperature anomalies under different climatic conditions Y. Aryal & S. Evans 10.1016/j.scitotenv.2023.162335
80. Air‐Sea Turbulent Heat Flux Feedback Over Mesoscale Eddies S. Moreton et al. 10.1029/2021GL095407
81. Using high-resolution global climate models from the PRIMAVERA project to create a European winter windstorm event set J. Lockwood et al. 10.5194/nhess-22-3585-2022
82. High‐resolution global climate simulations: Representation of cities D. Hertwig et al. 10.1002/joc.7018
83. U.K. Community Earth System Modeling for CMIP6 C. Senior et al. 10.1029/2019MS002004
84. Evaluating the climatic state of Indian Summer Monsoon during the mid-Pliocene period using CMIP6 model simulations K. Dahiya et al. 10.1016/j.dynatmoce.2024.101455
85. The surface downward longwave radiation of the CMIP6 HighResMIP in East Asia offline corrected by the three-dimensional sub-grid terrain longwave radiative effect scheme C. Gu et al. 10.1088/2515-7620/ad82b6
86. Future Projections and Uncertainties of CMIP6 for Hydrological Indicators and Their Discrepancies from CMIP5 over South Korea M. Doi & J. Kim 10.3390/w14182926
87. Modes of Atmospheric Energetics Based on HadGEM3-GC3.1-LL Simulations in the Framework of CMIP6 S. Michaelides & P. Salvador 10.1155/2023/3956086
88. Impacts of model resolution on responses of western North Pacific tropical cyclones to ENSO in the HighResMIP-PRIMAVERA ensemble J. Liu et al. 10.3389/feart.2023.1169885
89. An Approach to Link Climate Model Tropical Cyclogenesis Bias to Large‐Scale Wind Circulation Modes X. Feng et al. 10.1029/2023GL103838
90. Influence of horizontal resolution and complexity of aerosol–cloud interactions on marine stratocumulus and stratocumulus‐to‐cumulus transition in HadGEM3‐GC3.1 A. Ekman et al. 10.1002/qj.4494
91. Can we trust CMIP5/6 future projections of European winter precipitation? E. Moreno-Chamarro et al. 10.1088/1748-9326/abf28a
92. Evaluating the Water Cycle Over CONUS at the Watershed Scale for the Energy Exascale Earth System Model Version 1 (E3SMv1) Across Resolutions B. Harrop et al. 10.1029/2022MS003490
93. Evaluation of multi-season convection-permitting atmosphere – mixed-layer ocean simulations of the Maritime Continent E. Howard et al. 10.5194/gmd-17-3815-2024
94. Projections of mean and extreme precipitation over China and their resolution dependence in the HighResMIP experiments J. Liang et al. 10.1016/j.atmosres.2023.106932
95. Tropical Cyclone Integrated Kinetic Energy in an Ensemble of HighResMIP Simulations P. Kreussler et al. 10.1029/2020GL090963
96. Projected Future Changes in Tropical Cyclones Using the CMIP6 HighResMIP Multimodel Ensemble M. Roberts et al. 10.1029/2020GL088662
97. Climatological features of future MCSs over the Canadian Prairies using convection-permitting climate models Y. Hwang et al. 10.1016/j.atmosres.2023.106922
98. Responses and impacts of atmospheric rivers to climate change A. Payne et al. 10.1038/s43017-020-0030-5
99. Optimizing climate model selection in regional studies using an adaptive weather type based framework: a case study for extreme heat in Belgium F. Serras et al. 10.1007/s00382-024-07432-7
100. Evaluation of trends in extreme temperatures simulated by HighResMIP models across Europe A. Squintu et al. 10.1007/s00382-020-05596-6
101. Climate Change Signal in Atlantic Tropical Cyclones Today and Near Future C. Lee et al. 10.1029/2023EF003539
102. Evaluation of WRF model configurations for dynamic downscaling of tropical cyclones activity over the North Atlantic basin for Lagrangian moisture tracking analysis in future climate A. Pérez-Alarcón et al. 10.1016/j.atmosres.2024.107498
103. Statistical predictability of the Arctic sea ice volume anomaly: identifying predictors and optimal sampling locations L. Ponsoni et al. 10.5194/tc-14-2409-2020
104. Extreme rainfall and landslides as a response to human-induced climate change: a case study at Baixada Santista, Brazil, 2020 D. de Souza et al. 10.1007/s11069-024-06621-1
105. Deep mixed ocean volume in the Labrador Sea in HighResMIP models T. Koenigk et al. 10.1007/s00382-021-05785-x
106. Evaluation of extreme precipitation over Southeast Asia in the Coupled Model Intercomparison Project Phase 5 regional climate model results andHighResMIPglobal climate models M. Hariadi et al. 10.1002/joc.7938
107. Time-variations of the climate feedback parameter λ are associated with the Pacific Decadal Oscillation B. Meyssignac et al. 10.1038/s43247-023-00887-2
108. 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
109. Attribution of typhoon-induced torrential precipitation in Central Vietnam, October 2020 L. Luu et al. 10.1007/s10584-021-03261-3
110. Climatological features of future mesoscale convective systems in convection‐permitting climate models using CMIP6 and ERA5 in the central United States Y. Hwang et al. 10.1002/qj.4549
111. The disappearing Antilles Current dominates the weakening meridional heat transport in the North Atlantic Ocean under global warming J. Cai et al. 10.1088/1748-9326/ad3567
112. Evaluation of onset, cessation and seasonal precipitation of the Southeast Asia rainy season in CMIP5 regional climate models and HighResMIP global climate models M. Hariadi et al. 10.1002/joc.7404
113. European daily precipitation according to EURO-CORDEX regional climate models (RCMs) and high-resolution global climate models (GCMs) from the High-Resolution Model Intercomparison Project (HighResMIP) M. Demory et al. 10.5194/gmd-13-5485-2020
114. Model consistency for the underlying mechanisms for the Inter-decadal Pacific Oscillation-tropical Atlantic connection S. Yao et al. 10.1088/1748-9326/aca2bd
115. Impact of increased resolution on long-standing biases in HighResMIP-PRIMAVERA climate models E. Moreno-Chamarro et al. 10.5194/gmd-15-269-2022
116. Impact of increased resolution on the representation of the Canary upwelling system in climate models A. Sylla et al. 10.5194/gmd-15-8245-2022
117. Impact of Model Resolution on Tropical Cyclone Simulation Using the HighResMIP–PRIMAVERA Multimodel Ensemble M. Roberts et al. 10.1175/JCLI-D-19-0639.1
118. Will Increasing Climate Model Resolution Be Beneficial for ENSO Simulation? B. Liu et al. 10.1029/2021GL096932
119. Evaluation of CMIP6 HighResMIP for Hydrologic Modeling of Annual Maximum Discharge in Iowa A. Michalek et al. 10.1029/2022WR034166
120. The changes in the frequency of warm nights in Asia and the new climatic norms M. Kamangar & H. Shadman 10.1007/s00704-022-04183-5
121. Challenges simulating the AMOC in climate models L. Jackson et al. 10.1098/rsta.2022.0187
122. High-resolution modelling identifies the Bering Strait’s role in amplified Arctic warming G. Xu et al. 10.1038/s41558-024-02008-z
123. Impacts of Model Horizontal Resolution on Mean Sea Surface Temperature Biases in the Community Earth System Model G. Xu et al. 10.1029/2022JC019065
124. The benefits of high-resolution models in simulating the Kuroshio Extension and its long-term changes B. An et al. 10.1007/s00382-023-06862-z
125. BCC-CSM2-HR: a high-resolution version of the Beijing Climate Center Climate System Model T. Wu et al. 10.5194/gmd-14-2977-2021
126. Historical Simulations With HadGEM3‐GC3.1 for CMIP6 M. Andrews et al. 10.1029/2019MS001995
127. Evaluation of Mesoscale Convective Systems in Climate Simulations: Methodological Development and Results from MPAS-CAM over the United States Z. Feng et al. 10.1175/JCLI-D-20-0136.1
128. Fidelity of CMIP6 Models in Simulating June–September Rainfall Climatology, Spatial and Trend Patterns Over Complex Topography of Greater Horn of Africa W. Jima et al. 10.1007/s00024-023-03414-8
129. Long-term Regional Dynamic Sea Level Changes from CMIP6 Projections B. Ferrero et al. 10.1007/s00376-020-0178-4
130. Historical and future trends in South Asian monsoon low pressure systems in a high-resolution model ensemble S. Vishnu et al. 10.1038/s41612-023-00502-3
131. Evaluation of the CMCC global eddying ocean model for the Ocean Model Intercomparison Project (OMIP2) D. Iovino et al. 10.5194/gmd-16-6127-2023
132. Observed and Projected Changes in North Atlantic Seasonal Temperature Reduction and Their Drivers J. Grist et al. 10.1029/2023JC019837
133. Description of the resolution hierarchy of the global coupled HadGEM3-GC3.1 model as used in CMIP6 HighResMIP experiments M. Roberts et al. 10.5194/gmd-12-4999-2019
134. The Atlantic Meridional Overturning Circulation in High‐Resolution Models J. Hirschi et al. 10.1029/2019JC015522
135. Impact of Stochastic Physics and Model Resolution on the Simulation of Tropical Cyclones in Climate GCMs P. Vidale et al. 10.1175/JCLI-D-20-0507.1
136. A high-resolution perspective of extreme rainfall and river flow under extreme climate change in Southeast Asia M. Hariadi et al. 10.5194/hess-28-1935-2024
137. Predicting restoration and aquaculture potential of eastern oysters through an eco-physiological mechanistic model R. Lavaud et al. 10.1016/j.ecolmodel.2023.110603
138. ENSO Amplitude Asymmetry in Met Office Hadley Centre Climate Models S. Ineson et al. 10.3389/fclim.2021.789869
139. Prescreening-Based Subset Selection for Improving Predictions of Earth System Models With Application to Regional Prediction of Red Tide A. Elshall et al. 10.3389/feart.2022.786223
140. Impact of ocean resolution and mean state on the rate of AMOC weakening L. Jackson et al. 10.1007/s00382-020-05345-9
141. A Global Climate Model Performance Atlas for the Southern Hemisphere Extratropics Based on Regional Atmospheric Circulation Patterns S. Brands et al. 10.1029/2023GL103531
142. Boreal-winter teleconnections with tropical Indo-Pacific rainfall in HighResMIP historical simulations from the PRIMAVERA project F. Molteni et al. 10.1007/s00382-020-05358-4
143. Impact of Higher Spatial Atmospheric Resolution on Precipitation Extremes Over Land in Global Climate Models M. Bador et al. 10.1029/2019JD032184