Journal of Climate

Papers
(The H4-Index of Journal of Climate is 33. The table below lists those papers that are above that threshold based on CrossRef citation counts [max. 250 papers]. The publications cover those that have been published in the past four years, i.e., from 2021-04-01 to 2025-04-01.)
ArticleCitations
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The Interaction between the Nocturnal Amazonian Low-Level Jet and Convection in CESM184
Century-Scale Variability of Arctic SSH and Freshwater Content in a Past-1000-Year Model Experiment92
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The Role of Atmospheric Stabilities and Moisture Convergence in the Enhanced Dry Season Precipitation over Land from 1979 to 202174
Using the Observed Variations of the Start Date of the Rainy Season over Central America for Its Reliable Seasonal Outlook73
Rising Extreme Meltwater Trends in Greenland Ice Sheet (1950–2022): Surface Energy Balance and Large-Scale Circulation Changes69
Drivers of Biases in the CMIP6 Extratropical Storm Tracks. Part I: Northern Hemisphere64
Strong Coupling in Diurnal Variations of Clouds, Radiation, Winds, and Precipitation during the East Asian Summer Monsoon59
Why Is Climate Sensitivity for Solar Forcing Smaller than for an Equivalent CO2 Forcing?53
On the Role of Wind–Evaporation–SST Feedbacks in the Subseasonal Variability of the East Pacific ITCZ53
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Topographic Trapping of the Leeuwin Current and Its Impact on the 2010/11 Ningaloo Niño49
Deep Winter Mixed Layer Anchored by the Meandering Antarctic Circumpolar Current: Cross-Basin Variations48
Diversity of High-Frequency (10–25-Day) Boreal Summer Intraseasonal Oscillation over the Western North Pacific46
Disentangling North Atlantic Ocean–Atmosphere Coupling Using Circulation Analogs46
Subpolar North Atlantic Mean State Affects the Response of the Atlantic Meridional Overturning Circulation to the North Atlantic Oscillation in CMIP6 Models44
Comparing the Atmospheric Responses to Reduced Arctic Sea Ice, a Warmer Ocean, and Increased CO2 and Their Contributions to Projected Change at 2°C Global Warming43
Changes in the SST Seasonal Cycle in a Warmer North Pacific without Ocean Dynamical Feedbacks43
The Response of Tropopause-Overshooting Convection over North America to Climate Change41
A Physics-Informed Auto-Learning Framework for Developing Stochastic Conceptual Models for ENSO Diversity40
Reconstruction of Historical Site-Scale Dust Optical Depth (DOD) Time Series from Surface Dust Records and Satellite Retrievals in Northern China: Application to the Evaluation of DOD in CMIP6 Histori38
Role of the Spring Sea Surface Temperature over the Southeastern Indian Ocean in Bridging the Indian Ocean Dipole and Subsequent ENSO37
The Leading Modes of Northern Eurasian Winter Snowfall Variability and the Potential Influencing Factors37
Systematic Differences between the Northern and Southern Hemispheres: Warm-Frontal Ice Water Path Linked to the Origin of Extratropical Cyclones36
The Relationship between Convectively Coupled Waves and the East Pacific ITCZ36
Anomalous Northward Energy Transport due to Anthropogenic Aerosols during the Twentieth Century35
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Seasonal and Geographical Variations in Fundamental Weather Patterns during Extreme Precipitation as Identified from Omega Equation Forcing35
Interplay between Boreal Summer Intraseasonal Oscillation and Southern Hemisphere Stratospheric Polar Vortex Warming35
Evaluating the Performance of the North Pacific Victoria Mode as an ENSO Predictor Based on Multimodel Ensemble Hindcasts34
A Slower North Equatorial Countercurrent but Faster Equatorial Undercurrent in a Warming Climate34
The Importance and Responsibilities of Reviewers33
Lagrangian Overturning Pathways in the Eastern Subpolar North Atlantic33
A Surface Radiation Balance Dataset from Siple Dome in West Antarctica for Atmospheric and Climate Model Evaluation33
Clusters of Regional Precipitation Seasonality Change in the Community Earth System Model, Version 233
Comparisons between Short- and Long-Lived Cross-Equatorial Flow Events over the Maritime Continent: Perspective from the Intraseasonal Oscillation33
Nonlinear Radiative Response to Patterned Global Warming due to Convection Aggregation and Nonlinear Tropical Dynamics33
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