OOIR: Observatory of International Research

Papers

(The H4-Index of Climate Dynamics is 32. 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.)

Article	Citations
Revisiting the future changes in precipitation extremes over the Eastern Tibetan Plateau: from the thermodynamic–dynamic processes to model uncertainty	162
Explanatory framework of typhoon extreme wind speed predictions integrating the effects of climate changes	120
Multimodel GCM-RCM ensemble-based projections of tropical cyclone activities over CORDEX East Asia domain	113
Correction: Seasonal forecasting of the European North-West shelf seas: limits of winter and summer sea surface temperature predictability	103
Successive warm-wet and warm-dry events in the Great Lakes Basin: future projections using CMIP6 models	76
Cross-equatorial extension of the Pacific-South American wave train enabled by Southeastern South American rainfall	74
An evaluation of the seasonal Caribbean hydroclimate in low and high-resolution CESM and other CMIP6 models	63
Modulation of coupled Ural–Okhotsk circulation field on winter extreme cold events over East Asia	57
The impact of vertical model levels on the prediction of MJO teleconnections. Part II: The stratospheric pathway in the UFS global coupled model	52
Correction to: Dynamical controls on the diurnal cycle of temperature in complex topography	48
Correction: Local and synoptic mechanisms causing Southern California’s Santa Ana winds	48
Correction: Relationship between south Asian summer monsoon intensity and north Indian ocean tropical cyclone activity	46
Impact of climate change on frequency and community structure of red tide events in the northern South China Sea	45
Comparative analysis of east Asian summer monsoon northern boundary indices: variability, climate anomalies and driving mechanisms	45
Correction: Maritime Continent salinity as a new predictor for south Asian summer monsoon rainfall	44
Advancing effective radius parameterizations in climate models: insights from fundamental theoretical studies and CMIP6 model	43
Seasonality of feedback mechanisms involved in Pacific coastal Niño events	42
Tropospheric winds over West Sumatra—a comparison between ERA-5 reanalysis and equatorial atmosphere radar	41
Sensitivity of initial soil moisture in simulating a heatwave event over India	41
A winter cold nights pattern in the Northern Hemisphere lands: Circum–hemisphere teleconnection of extreme cold events	40
Impacts of model resolution on the simulation of sea-level variability by a global ocean-sea ice model	40
Trends in precipitable water vapor in North America based on GNSS observation and ERA5 reanalysis	39
Taxus tree-ring chronologies from southern England reveal western European hydroclimate changes over the past three centuries	38
Representing low temperature events and uncovering their dynamics in China between 1979 and 2018 amid climate change	38
The role of the land surface for surface climate: results from a stepwise land–atmosphere coupling experiment	38

Comparative analysis of high-resolution CMIP6 GCM and CMIP5 RCM: unveiling biases and advancements in simulating compound extreme events in China	37
Precipitation variability in CMIP6 climate models across the North Atlantic–European region and their Links to Atmospheric Circulation	36
Upper ocean salinity and temperature changes and their contributions to the stratification in the tropical Pacific under global warming	35
Interplay of anthropogenic and natural drivers of observed coupled sea surface temperature - Arctic sea ice variability	35
Tele-connected rainfall extremes over West and East Asia in April 2024 tied to Indian Ocean heating	34
Spatio-temporal evolution of compound hot and dry extremes synchronizations in Europe	33
Simulated millennial-scale climate variability driven by a convection–advection oscillator	32
Summer precipitation responses to CO2 removal scenario over the transitional climate zone in East Asia and the driving mechanisms	32