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The improvements of sea surface temperature simulation over China Offshore Sea in present climate from CMIP5 to CMIP6 models
By using the 43 Historical experiments from phase 6 of the Coupled Model Intercomparison Project (CMIP6) and 45 Historical experiments from phase 5...
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On the spring stratospheric final warming in CMIP5 and CMIP6 models
This study evaluates the performance in simulating the stratospheric final warming events (SFWs) that lead to the final collapse of the stratospheric...
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Evaluation of ENSO in CMIP5 and CMIP6 models and its significance in the rainfall in Northeast Thailand
El Niño Southern Oscillation (ENSO) is a significant form of internal climate variability resulting from the interactions between the atmosphere and...
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Weak persistence of Northwest Pacific anomalous anticyclone during post-El Niño summers in CMIP5 and CMIP6 models
An anomalous anticyclone (AAC) recurs over the Indo-Northwest Pacific during post-El Niño summers, regulating climate anomalies in the densely...
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Regional climate projections of daily extreme temperatures in Argentina applying statistical downscaling to CMIP5 and CMIP6 models
Argentina is a country with a variety of climates, where an increase in mean and extreme temperatures is currently on-going, demanding regional...
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Solar radiation variability across Nigeria’s climatic zones: a validation and projection study with CORDEX, CMIP5, and CMIP6 models
Harnessing energy from the sun is crucial for locations battling with energy poverty and generation, especially in Africa, where equity in energy...
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Low-level circulation over Central Equatorial Africa as simulated from CMIP5 to CMIP6 models
We evaluate and compare the simulation of the main features (low-level westerlies (LLWs) and the Congo basin (CB) cell) of low-level circulation in...
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On the simulation of northeast monsoon rainfall over southern peninsular India in CMIP5 and CMIP6 models
Northeast monsoon rainfall (Oct–Dec) over southern peninsular India (NEMR-SP) has the high coefficient of variation (26%) and low predictability. The...
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The simulation of the Indo-Pacific warm pool SST warming trend in CMIP5 and CMIP6
This paper evaluates Indo-Pacific warm pool (IPWP) sea surface temperature (SST) warming biases of Coupled Model Intercomparison Project Phase 5...
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Model uncertainty in synoptic circulation patterns and precipitation changes in Southern South America using CMIP5 and CMIP6 models
The effects of global warming on the regional climate of southern South America (SSA) during the recent decades have been exhaustively documented...
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How Well Do CMIP6 and CMIP5 Models Simulate the Climatological Seasonal Variations in Ocean Salinity?
This paper includes a comprehensive assessment of 40 models from the Coupled Model Intercomparison Project phase 5 (CMIP5) and 33 models from the...
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Comparisons between CMIP5 and CMIP6 models in simulations of the climatology and interannual variability of the east asian summer Monsoon
The climatology and interannual variability of East Asian summer monsoon (EASM) is evaluated based on the outputs from the phase 6 of the Coupled...
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Multiscale evaluation of CMIP5 models using wavelet-based descriptive and diagnostic techniques
Time–frequency localization of model-data discrepancies may provide useful information for climate models inter-comparison, and especially for the...
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Relative performance of CMIP5 and CMIP6 models in simulating rainfall in Peninsular Malaysia
This study evaluated the skills of global climate models (GCMs) of the fifth and sixth Coupled Model Intercomparison Project (CMIP5 and CMIP6) in...
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Selection of multiple ensemble representative CMIP5 climate models for climate change study in develo** river basin: the case of Awash River Basin, Ethiopia
The aim of this investigation is to identify a representative set of climate model projections for the Awash Basin using accessible general...
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Comparison of GCMs Under CMIP5 and CMIP6 in Reproducing Observed Precipitation in Ethiopia During Rainy Seasons
Model selection over a region known with data scarcity is crucial to get a substitute to study trends, variability and projections. This study was...
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Association of the cloud radiative effect with the changes in the northern edge of Hadley circulation between the CMIP5 and CMIP6 models in boreal summer
In this study, the relationship between the cloud radiative effect and the northern boundary of the Hadley circulation (HC) in summer is analyzed...
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Evaluation of the seasonal to decadal variability in dynamic sea level simulations from CMIP5 to CMIP6
Previous studies have revealed little progress in the ensemble mean of Coupled Model Intercomparison Project Phase 6 (CMIP6) models compared to Phase...
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Biases and improvements of the ENSO-East Asian winter monsoon teleconnection in CMIP5 and CMIP6 models
The influence of El Niño–Southern Oscillation (ENSO) on the East Asian winter monsoon (EAWM) is investigated based on the outputs of phase 6 of the...
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Atmospheric Centers of Action in the Northern Hemisphere: Current Features and Expected Changes in the 21st Century Based on Simulations with the CMIP5 and CMIP6 Ensembles of Climate Models
AbstractRegional features of global climate changes are significantly related to the regimes of atmospheric centers of action (ACA) and their...
