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Multi-decadal streamflow projections for catchments in Brazil based on CMIP6 multi-model simulations and neural network embeddings for linear regression models
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The contribution of climate change to increasing extreme ocean warming around Japan
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2022
Huard, David, Fyke, Jeremy, et al.
Estimating the Likelihood of GHG Concentration Scenarios From Probabilistic Integrated Assessment Model Simulations
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2022
Hayashi, Michiya, Shiogama, Hideo
Assessment of CMIP6-based future climate projections selected for impact studies in Japan
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2022
Worou, Koffi, Goosse, Hugues, et al.
Weakened impact of the Atlantic Niño on the future equatorial Atlantic and Guinea Coast rainfall
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2021
T.H.J. Hermans, C.A. Katsman, et al.
The Effect of Wind Stress on Seasonal Sea-Level Change on the Northwestern European Shelf
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Diverse Responses of Global‐Mean Surface Temperature to External Forcings and Internal Climate Variability in Observations and CMIP6 Models
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Lim Kam Sian, Kenny Thiam Choy, Wang, Jianhong, et al.
Multi-Decadal Variability and Future Changes in Precipitation over Southern Africa
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2021
Kajtar, Jules B., Santoso, Agus, et al.
CMIP5 Intermodel Relationships in the Baseline Southern Ocean Climate System and With Future Projections
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2021
Purich, Ariaan, England, Matthew H.
Historical and Future Projected Warming of Antarctic Shelf Bottom Water in CMIP6 Models
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2021
McBride, Laura A., Hope, Austin P., et al.
Comparison of CMIP6 historical climate simulations and future projected warming to an empirical model of global climate
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2021
Koch, Alexander, Hubau, Wannes, et al.
Earth System Models Are Not Capturing Present‐Day Tropical Forest Carbon Dynamics
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2021
Nicholls, Zebedee, Lewis, Jared, et al.
Regionally aggregated, stitched and de‐drifted CMIP‐climate data, processed with netCDF‐SCM v2.0.0
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2021
Sledd, Anne, L’Ecuyer, Tristan
Uncertainty in Forced and Natural Arctic Solar Absorption Variations in CMIP6 Models
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2021
Hayashi, Michiya, Shiogama H., et al.
The northwestern Pacific warming record in August 2020 occurred under anthropogenic forcing
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