Geophysical Research Letters

Papers
(The H4-Index of Geophysical Research Letters is 61. 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 2020-11-01 to 2024-11-01.)
ArticleCitations
Warmer and Drier Fire Seasons Contribute to Increases in Area Burned at High Severity in Western US Forests From 1985 to 2017284
Increase in Compound Drought and Heatwaves in a Warming World170
Record‐Breaking Meiyu Rainfall Around the Yangtze River in 2020 Regulated by the Subseasonal Phase Transition of the North Atlantic Oscillation163
Global Propagation of Ionospheric Disturbances Associated With the 2022 Tonga Volcanic Eruption157
Enhanced Meiyu‐Baiu Rainfall in Early Summer 2020: Aftermath of the 2019 Super IOD Event139
A Unified Clumped Isotope Thermometer Calibration (0.5–1,100°C) Using Carbonate‐Based Standardization139
Hydrogen Wettability of Sandstone Reservoirs: Implications for Hydrogen Geo‐Storage135
Stereo Plume Height and Motion Retrievals for the Record‐Setting Hunga Tonga‐Hunga Ha'apai Eruption of 15 January 2022119
On the Covariation of Chlorophyll Fluorescence and Photosynthesis Across Scales118
The Hunga Tonga‐Hunga Ha'apai Hydration of the Stratosphere115
The 15 January 2022 Hunga Tonga Eruption History as Inferred From Ionospheric Observations114
Satellite and Ocean Data Reveal Marked Increase in Earth’s Heating Rate114
Numerical Simulation of Atmospheric Lamb Waves Generated by the 2022 Hunga‐Tonga Volcanic Eruption112
Worldwide Signature of the 2022 Tonga Volcanic Tsunami110
Rapid Characterization of Large Volcanic Eruptions: Measuring the Impulse of the Hunga Tonga Ha’apai Explosion From Teleseismic Waves101
Mapping Forest Height and Aboveground Biomass by Integrating ICESat‐2, Sentinel‐1 and Sentinel‐2 Data Using Random Forest Algorithm in Northwest Himalayan Foothills of India97
Rapid Conjugate Appearance of the Giant Ionospheric Lamb Wave Signatures in the Northern Hemisphere After Hunga‐Tonga Volcano Eruptions94
Annual Mean Arctic Amplification 1970–2020: Observed and Simulated by CMIP6 Climate Models92
Differing Mechanisms of New Particle Formation at Two Arctic Sites87
Five Decades of Observed Daily Precipitation Reveal Longer and More Variable Drought Events Across Much of the Western United States86
The Longest 2020 Meiyu Season Over the Past 60 Years: Subseasonal Perspective and Its Predictions86
How Does El Niño–Southern Oscillation Change Under Global Warming—A First Look at CMIP684
Changing Lengths of the Four Seasons by Global Warming82
Moisture Sources and Transport for Extreme Precipitation Over Henan in July 202180
Relativistic Electron Microbursts as High‐Energy Tail of Pulsating Aurora Electrons79
Warming and Freshening of the Pacific Inflow to the Arctic From 1990‐2019 Implying Dramatic Shoaling in Pacific Winter Water Ventilation of the Arctic Water Column79
The Extreme Positive Indian Ocean Dipole of 2019 and Associated Indian Summer Monsoon Rainfall Response78
Using Machine Learning to Analyze Physical Causes of Climate Change: A Case Study of U.S. Midwest Extreme Precipitation76
Global Changes in 20‐Year, 50‐Year, and 100‐Year River Floods76
Impacts of the January 2022 Tonga Volcanic Eruption on the Ionospheric Dynamo: ICON‐MIGHTI and Swarm Observations of Extreme Neutral Winds and Currents75
Do CMIP6 Climate Models Simulate Global or Regional Compound Events Skillfully?73
Rapidly Evolving Controls of Landslides After a Strong Earthquake and Implications for Hazard Assessments73
Systematic Climate Model Biases in the Large‐Scale Patterns of Recent Sea‐Surface Temperature and Sea‐Level Pressure Change73
Where Are Global Vegetation Greening and Browning Trends Significant?73
Long‐Term (1979‐Present) Total Water Storage Anomalies Over the Global Land Derived by Reconstructing GRACE Data72
Historical and Projected Changes in the Southern Hemisphere Surface Westerlies72
Distributed Global Debris Thickness Estimates Reveal Debris Significantly Impacts Glacier Mass Balance72
Subsurface Multi‐Physical Monitoring of a Reservoir Landslide With the Fiber‐Optic Nerve System71
Spatial Patterns and Drivers of Nonperennial Flow Regimes in the Contiguous United States71
Trends in Global Tropical Cyclone Activity: 1990–202170
The Recent Emergence of Arctic Amplification70
Subsurface Evolution and Persistence of Marine Heatwaves in the Northeast Pacific70
Atlantic Deep Water Formation Occurs Primarily in the Iceland Basin and Irminger Sea by Local Buoyancy Forcing70
Holocene Monsoon Change and Abrupt Events on the Western Chinese Loess Plateau as Revealed by Accurately Dated Stalagmites70
Increasing Synchronous Fire Danger in Forests of the Western United States69
Mars Climate Sounder Observation of Mars' 2018 Global Dust Storm69
The Seasonal and Regional Transition to an Ice‐Free Arctic68
Space‐Borne Cloud‐Native Satellite‐Derived Bathymetry (SDB) Models Using ICESat‐2 And Sentinel‐268
New Precise Dating of the India‐Asia Collision in the Tibetan Himalaya at 61 Ma67
A Shorter, Sharper Rainy Season Amplifies California Wildfire Risk67
Coseismic and Early Postseismic Deformation Due to the 2021 M7.4 Maduo (China) Earthquake66
Global Increases in Compound Flood‐Hot Extreme Hazards Under Climate Warming65
Surface Melt and Runoff on Antarctic Ice Shelves at 1.5°C, 2°C, and 4°C of Future Warming65
Record Low Antarctic Sea Ice Cover in February 202265
Persistent Stratospheric Warming Due to 2019–2020 Australian Wildfire Smoke64
The TSIS‐1 Hybrid Solar Reference Spectrum63
Variation in Concentration and Sources of Black Carbon in a Megacity of China During the COVID‐19 Pandemic63
Compound Extremes Drive the Western Oregon Wildfires of September 202062
Chinese Regulations Are Working—Why Is Surface Ozone Over Industrialized Areas Still High? Applying Lessons From Northeast US Air Quality Evolution61
Global Ocean Mass Change From GRACE and GRACE Follow‐On and Altimeter and Argo Measurements61
Observed Impacts of COVID‐19 on Urban CO2 Emissions61
A Multivariate Flash Drought Indicator for Identifying Global Hotspots and Associated Climate Controls61
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