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Mid-Holocene global monsoon area and precipitation from PMIP simulations
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Liu Y., Jiang D.
Mid-Holocene permafrost: Results from CMIP5 simulations
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Physical Mechanisms of Tropical Climate Feedbacks Investigated using Temperature and Moisture Trends
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da Silva G. A., Mendes D.
Refinement of the daily precipitation simulated by the CMIP5 models over the north of the Northeast of Brazil
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Melet A. V., Meyssignac B.
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Robust Sahel drought due to the Interdecadal Pacific Oscillation in CMIP5 simulations
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DeAngelis A. M., Qu X., et al.
An observational radiative constraint on hydrologic cycle intensification
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Glacial Atlantic overturning increased by wind stress in climate models
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Systematic change in global patterns of streamflow following volcanic eruptions
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Arctic summer storm track in CMIP3/5 climate models
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multimodel ensemble pattern regression method to correct the tropical Pacific SST change pattern under global warming
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New Perspectives on Observed and Simulated Antarctic Sea Ice Extent Trends Using Optimal Fingerprinting Techniques
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Climate Model Dependence and the Ensemble Dependence Transformation of CMIP Projections
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Arctic summer storm track in CMIP3/5 climate models
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Seasonal changes in tropical SST and the surface energy budget under global warming projected by CMIP5 models
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Impacts of External Forcing on the Decadal Climate Variability in CMIP5 Simulations
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Robust Forced Response in South Asian Summer Monsoon in a Future Climate
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Cavaleri M. A., Reed S. C., et al.
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Bezeau P., Sharp M., et al.
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Oliveira G., Lima-Ribeiro M., et al.
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Solar signals in CMIP-5 simulations: The ozone response
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Chan D., Wu Q.
Attributing Observed SST Trends and Sub-Continental Land Warming to Anthropogenic Forcing during 1979-2005
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Asian summer monsoon onset in simulations and CMIP5 projections using four Chinese climate models
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Improving climate change detection through optimal seasonal averaging: the case of the North Atlantic jet and European precipitation
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Koppen bioclimatic evaluation of CMIP historical climate simulations
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Is the tropical atmosphere in convective quasi-equilibrium?
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