Journal of Geophysical Research-Atmospheres

Papers
(The H4-Index of Journal of Geophysical Research-Atmospheres is 35. 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 2022-01-01 to 2026-01-01.)
ArticleCitations
94
Global Temperature Forecasting Incrementally Improved by Model Output Statistics92
Impacts of El Niño‐Southern Oscillation on Earth's Radiant Energy Budget79
76
Reasons for Low Fraction of Arctic Stratospheric Cloud in 2014/2015 Winter74
Cloud Condensation Nuclei Closure Study Using Airborne Measurements Over the Southern Great Plains63
The Effect of Physically Based Ice Radiative Processes on Greenland Ice Sheet Albedo and Surface Mass Balance in E3SM61
Issue Information60
The Impact of Assimilating X‐Band Phased Array and S‐Band Radar Data on the Forecast of Tropical Cyclone Saola (2023)54
54
Fusion of MISR Stereo Cloud Heights and Terra‐MODIS Thermal Infrared Radiances to Estimate Two‐Layered Cloud Properties49
Intensity and Structural Changes During the Eyewall Replacement Cycle of Typhoon Khanun (2023) Observed by Five POES Microwave Imagers49
Long‐Emission‐Wavelength Humic‐Like Component (L‐HULIS) as a Secondary Source Tracer of Brown Carbon in the Atmosphere48
Variations in Tropical Cyclone Size and Rainfall Patterns Based on Synoptic‐Scale Moisture Environments in the North Atlantic48
Extreme Compound and Seesaw Hydrometeorological Events in New Zealand: An Initial Assessment47
Characteristics of the Mediterranean Cyclone IANOS in Convection‐Permitting Simulations: Unraveling Model Sensitivity to Microphysics and Cumulus Parameterization47
Synchronous Tropical Andean Hydroclimate Variability During the Last Millennium47
Synchronization of the Recent Decline of East African Long Rains and Northwestern Eurasian Warming46
Revisiting the Contributions of Surface Sensible and Latent Heat Fluxes to the Outer Spiral Rainbands of Tropical Cyclones46
Trends in Oceanic Precipitation Characteristics Inferred From Shipboard Present‐Weather Reports, 1950–201945
Intensified Atmospheric Branch of the Hydrological Cycle Over the Tibetan Plateau During the Last Interglacial From a Dynamical Downscaling Perspective45
Response of Moist Convection to the Spectral Feature of the Surface Flux Field at Model Resolution Across the Gray Zone43
A Regional Air‐Sea Coupled Model Developed for the East Asia and Western North Pacific Monsoon Region43
Non‐Gaussian Distributions of TOA SW Flux as Observed by MISR and CERES41
Issue Information40
Issue Information40
The Impact of Oceanic Feedbacks on Stratosphere‐Troposphere Coupling in an Idealized Model39
What Controls the Subseasonal Precipitation Reversal Over the Western Tibetan Plateau in Winter?39
Simulations of the North Tropical Atlantic Mode–ENSO Connection in CMIP5 and CMIP6 Models39
Evaluation and Improvement of the ECMWF Aviation Turbulence Forecasts37
A Scheme for Representing Aromatic Secondary Organic Aerosols in Chemical Transport Models: Application to Source Attribution of Organic Aerosols Over South Korea During the KORUS‐AQ Campaign36
Near‐Storm Environmental Relationships With Tropical Oceanic Convective Structure Observed During NASA CPEX and CPEX‐AW36
The Importance of NOx Control for Peak Ozone Mitigation Based on a Sensitivity Study Using CMAQ‐HDDM‐3D Model During a Typical Episode Over the Yangtze River Delta Region, China36
WRF Simulations of Future Saharan Dust Concentrations Across West Africa: Historical and Late 21st Century36
Prolonged Atmospheric Chemical Lifetime of Unsaturated Fatty Acids From Cooking Sources Observed in Beijing During Wintertime36
An Evaluation of Cloud‐Precipitation Structures in Mixed‐Phase Stratocumuli Over the Southern Ocean in Kilometer‐Scale ICON Simulations During CAPRICORN35
Dependence of Cloud Macrophysical Properties and Phase Distributions on Environmental Conditions Over the North Atlantic and Southern Ocean: Results From COMBLE and MARCUS35
Impacts of North Atlantic Model Biases on Natural Decadal Climate Variability35
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