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Quantifying the Added Value in the NEX-GDDP-CMIP6 Models as Compared to Native CMIP6 in Simulating Africa’s Diverse Precipitation Climatology
In the era of Anthropocene climate that the world is currently experiencing, accurate climate models that exhibit minimal uncertainties for precise...
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Performance of CMIP6 models over South America
Assessing the performance of global climate models in the present is essential to attribute confidence to their future projections. This work aims to...
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CMIP6 Model Evaluation for Mean and Extreme Precipitation Over India
Extreme precipitation is typical in the Indian subcontinent, and these occurrences might cause human fatalities, property damage, and 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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Performance evaluation of CMIP6 in simulating extreme precipitation in Madagascar
This study assesses the performance of 37 global climate models (GCMs) from the Coupled Model Inter-comparison Project Phase 6 (CMIP6) in simulating...
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Attribution of Biases of Interhemispheric Temperature Contrast in CMIP6 Models
One of the basic characteristics of Earth’s modern climate is that the Northern Hemisphere (NH) is climatologically warmer than the Southern...
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Tropical atlantic climate biases and DAMIP experiments: insights from CMIP6 models
This study investigates the representation of the Tropical Atlantic zonal and meridional modes of sea surface temperature variability, as well as...
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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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Simulation of extreme precipitation changes in Central Asia using CMIP6 under different climate scenarios
Central Asia has a dry climate, scarce water resources, extremely fragile ecosystems, and frequent extreme precipitation events. Using the data of 22...
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Evaluation and Projection of Extreme High Temperature Indices in Southwestern China Using NEX-GDDP-CMIP6
Based on the recently released NASA Earth Exchange Global Daily Downscaled Projections (NEX-GDDP) Coupled Model Intercomparison Project Phase 6...
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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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Interdecadal tropical Pacific–Atlantic interaction simulated in CMIP6 models
The interaction between the tropical Pacific and Atlantic at the decadal timescale has received widespread attention. This study evaluates the...
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Assessing the Performance of CMIP6 Models in Simulating Droughts across Global Drylands
Both the attribution of historical change and future projections of droughts rely heavily on climate modeling. However, reasonable drought...
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Evaluation and attribution of shortwave feedbacks to ENSO in CMIP6 models
The shortwave (SW) feedback to El Niño–Southern Oscillation (ENSO) is one of the largest biases in climate models, as the feedback includes...
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CMIP6 model evaluation for sea surface height responses to ENSO
El Niño-Southern Oscillation (ENSO) exhibits a substantial impact on sea surface height (SSH), and some climate models are significantly biased in...
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Robustness of precipitation Emergent Constraints in CMIP6 models
An Emergent Constraint (EC) is a physically-explainable relationship between model simulations of a past climate variable (predictor) and projections...
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Climate change projections in Guatemala: temperature and precipitation changes according to CMIP6 models
Projected changes in precipitation and temperature for Guatemala were examined using the phase 6 dataset of the Coupled Model Intercomparison Project...
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Understanding of CMIP6 surface temperature cold bias over the westerly and monsoon regions of the Tibetan Plateau
The Tibetan Plateau (TP) directly heats the middle tropospheric atmosphere, and accurate simulation of its surface temperature is of great concern...
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Simulations and Projections of Winter Sea Ice in the Barents Sea by CMIP6 Climate Models
Dramatic changes in the sea ice characteristics in the Barents Sea have potential consequences for the weather and climate systems of mid-latitude...
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Evaluation of CMIP6 model skills in simulating tropical climate extremes over Malawi, Southern Africa
Malawi, a develo** country in southeast Africa, is one of the most vulnerable countries to climate change and associated impacts. Availability of...
