Land Use/Cover Change Impacts in CMIP5 Climate Simulations %u2013A New Methodology and 21st Century Challenges
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2013
Harvey B., Shaffrey L., et al.
Equator-to-pole temperature differences and the extra-tropical storm track responses of the CMIP5 climate models
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2013
Anstey J. A., Davini P., et al.
Multi-model analysis of Northern Hemisphere winter blocking: Model biases and the role of resolution
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Assessment of Southern Ocean mixed layer depths in CMIP5 models: historical bias and forcing response
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2013
Blazquez J., Nu�ez M. N.
Analysis of uncertainties in future climate projections for South America: comparison of WCRP-CMIP3 and WCRP-CMIP5 models.
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2013
Yang X., Rosati A., et al.
A predictable AMO-like pattern in GFDL's fully-coupled ensemble initialization and decadal forecasting system
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2013
Xiao C., Zhang Y.
Simulation of the Westerly Jet Axis in Boreal Winter by the Climate System Model FGOALS-g2
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The Flexible Global Ocean-Atmosphere-Land System Model: Grid-point Version 2: FGOALS-g2
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2013
Collier M. A., Rotstayn L. D., et al.
Ocean circulation response to anthropogenic-aerosol and greenhouse-gas forcing in the CSIRO-Mk3.6.0 coupled climate model
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Asymmetry in the IOD and ENSO Teleconnection in a CMIP5 Model Ensemble and Its Relevance to Regional Rainfall
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2013
Weller E., Cai W.
Realism of the Indian Ocean Dipole in CMIP5 models: the implication for climate projections
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2013
Joetzjer E., Douville H., et al.
Present-day and future Amazonian precipitation in global climate models: CMIP5 versus CMIP3
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2013
Chiang J. C., Chang C., et al.
Long-Term Behavior of the Atlantic Interhemispheric SST Gradient in the CMIP5 Historical Simulations
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Projections of heavy rainfall over the central United States based on CMIP5 models
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2013
Seo K., Ok J., et al.
Assessing future changes in the East Asian summer monsoon using CMIP5 coupled models
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2013
Sabeerali C. T., Dandi R. A., et al.
Simulation of boreal summer intraseasonal oscillations in the latest CMIP5 coupled GCMs
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2013
Aloysius N. R., Sheffield J., et al.
Global Bias-corrected and Downscaled Climate Grids for the 20th and 21st Centuries Based on CMIP5: Application to the Congo Basin
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2013
Dwyer J. G., Biasutti M., et al.
The effect of greenhouse-gas-induced changes in SST on the seasonality of tropical precipitation
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2013
Smith I. N., Syktus J., et al.
The relative performance of Australian CMIP5 models based on rainfall and ENSO metrics
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2013
Ramirez-Villegas J., Challinor A. J., et al.
Implications of regional improvement in global climate models for agricultural impact research
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2013
Dufresne J., Foujols M., et al.
Climate change projections using the IPSL-CM5 Earth System Model: from CMIP3 to CMIP5
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Water vapor transport and cross-equatorial flow over the Asian-Australia monsoon region simulated by CMIP5 climate models
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2013
Cagnazzo C., Manzini E., et al.
Role of stratospheric dynamics in the ozone%u2013carbon connection in the Southern Hemisphere
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Application of regularised optimal fingerprinting to attribution. Part I: method, properties, and idealised analysis
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2013
Ribes A., Terray L.
Application of regularised optimal fingerprinting to attribution. Part II: application to global near-surface temperature based on CMIP5 simulations
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On the spread of changes in marine low cloud cover in climate model simulations of the 21st century
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2013
Hosking J., Orr A., et al.
The influence of the Amundsen-Bellingshausen Seas Low on the climate of West Antarctica and its representation in coupled climate model simulations
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2013
Torres R. R., Marengo J. A.
Climate change hotspots over South America: from CMIP3 to CMIP5 multi-model datasets
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2013
Jiang D., Tian Z.
East Asian monsoon change for the 21st century: Results of CMIP3 and CMIP5 models
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2013
Ylh?isi J. S., Garr? L., et al.
Quantifying sources of climate uncertainty to inform risk analysis for climate change decision-making
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Consequences of poor representation of Arctic sea-ice albedo and cloud-radiation interactions in the CMIP5 model ensemble
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2013
Izumi K., Bartlein P. J., et al.
Consistent behaviour of the climate system in response to past and future forcing.
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2013
Li G., Harrison S. P., et al.
Precipitation scaling with temperature in warm and cold climates: an analysis of CMIP5 simulations.
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Evaluation of drought indices at interannual to climate change timescales: A case study over the Amazon and Mississippi river basins.
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2013
Toreti A., Naveau P., et al.
Projections of global changes in precipitation extremes from Coupled Model Intercomparison Project Phase 5 models
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2013
Purich A., Cowan T., et al.
Autumn Precipitation Trends over Southern Hemisphere Midlatitudes as Simulated by CMIP5 Models
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Uncertainties on the simulated summer precipitation over Eastern China from the CMIP5 models
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2013
Niznik M. J., Lintner B. R.
Circulation, moisture, and precipitation relationships along the South Pacific Convergence Zone in reanalyses and CMIP5 models
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2013
Mitchell D. M., Stott P. A., et al.
The impact of stratospheric resolution on the detectability of climate change signals in the free atmosphere
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Limited Evidence of Anthropogenic Influence on the 2011-12 Extreme Rainfall over Southeast Australia
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2013
Hanasaki N., Fujimori S., et al.
A global water scarcity assessment under Shared Socio-economic Pathways %u2013 Part 2: Water availability and scarcity
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2013
Rupp D. E., Abatzoglou J. T., et al.
Evaluation of CMIP5 20th century climate simulations for the Pacific Northwest USA
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2013
Santoso A., McGregor S., et al.
Late-twentieth-century emergence of the El Nino propagation asymmetry and future projections
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Why is the amplitude of the Indian Ocean Dipole overly large in CMIP3 and CMIP5 climate models?
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2013
Cowan T., Cai W.
The response of the large-scale ocean circulation to 20th century Asian and non-Asian aerosols
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2013
Cowan T., Cai W., et al.
Forcing of anthropogenic aerosols on temperature trends of the sub-thermocline southern Indian Ocean
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2013
Lutz A. F., Immerzeel W. W., et al.
Comparison of climate change signals in CMIP3 and CMIP5 multi-model ensembles and implications for Central Asian glaciers
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2013
Young P. J., Bulter A. H., et al.
Agreement in late twentieth century Southern Hemisphere stratospheric temperature trends in observations and CCMVal-2, CMIP3, and CMIP5 models
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An explanation for the difference between twentieth and twenty-first century land%u2013sea warming ratio in climate models
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2013
Lavers D. A., Allan R. P., et al.
Future changes in atmospheric rivers and their implications for winter flooding in Britain
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2013
Zunz V., Goosse H., et al.
How does internal variability influence the ability of CMIP5 models to reproduce the recent trend in Southern Ocean sea ice extent?
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