Delays reducing waterborne and water-related infectious diseases in China under climate change
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2014
Lebsock M. D., Su H.
Application of Active Spaceborne Remote Sensing for Understanding Biases Between Passive Cloud Water Path Retrievals
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2014
Ding Y., Carton J. A., et al.
Ocean response to volcanic eruptions in Coupled Model Intercomparison Project 5 (CMIP5) simulations
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2014
Grise K. M., Polvani L. M.
Southern Hemisphere cloud-dynamics biases in CMIP5 models and their implications for climate projections
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2014
Grise K. M., Polvani L. M.
The response of midlatitude jets to increased CO2: Distinguishing the roles of sea surface temperature and direct radiative forcing
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2014
Sperber K. R., Annamalai H.
The Use of Fractional Accumulated Precipitation for the Evaluation of the Annual Cycle of Monsoons
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Evaluation of pan-Arctic melt-freeze onset in CMIP5 climate models and reanalyses using surface observations
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2014
Qu X., Huang G., et al.
Consistent responses of East Asian summermean rainfall to global warming in CMIP5 simulations
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2014
Zappa G., Masato G., et al.
Linking Northern Hemisphere blocking and storm track biases in the CMIP5 climate models
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The response of the Southern Hemispheric eddy-driven jet to future changes in shortwave radiation in CMIP5
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2014
Kamae Y., Watanabe M., et al.
Summertime land-sea thermal contrast and atmospheric circulation over East Asia in a warming climate. Part I: Past changes and future projections
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2014
Kamae Y., Watanabe M., et al.
Summertime land-sea thermal contrast and atmospheric circulation over East Asia in a warming climate-Part II: Importance of CO2-induced continental warming
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2014
Kamae Y., Shiogama H., et al.
Attributing the increase in Northern Hemisphere hot summers since the late 20th century
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2014
Ma Q., Wang K., et al.
Evaluations of Atmospheric Downward Longwave Radiation from 44 Coupled General Circulation Models of CMIP5
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2014
Wang K.
Measurement Biases Explain Discrepancies between the Observed and Simulated Decadal Variability of Surface Incident Solar Radiation
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2014
Chadwick R. S., Good P., et al.
Surface warming patterns drive tropical rainfall pattern responses to CO2 forcing on all timescales
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2014
Cabre A., Marinov I., et al.
Consistent global responses of marine ecosystems to future climate change across the IPCC AR5 earth system models
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2014
Cattiaux J., Douville H., et al.
Projected increase in diurnal and inter-diurnal variations of European summer temperatures
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2014
Wjcik R.
Reliability of the CMIP5 GCM simulations in reproducing atmospheric circulation over Europe and the North Atlantic: a statistical downscaling perspective
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2014
Freedman F. R., Pitts K. L., et al.
Evaluation of CMIP climate model hydrological output for the Mississippi River Basin using GRACE satellite observations
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Sources of uncertainty in projections of twenty-first century westerly wind changes over the Amundsen Sea, West Antarctica, in CMIP5 climate models
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2014
Hajima T., Tachiiri K., et al.
Uncertainty of Concentration - Terrestrial Carbon Feedback in Earth System Models
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Projections of global changes in precipitation extremes from Coupled Model Intercomparison Project Phase 5 models
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2014
Arnell N. W., Lloyd-Hughes B.
The global-scale impacts of climate change on water resources and flooding under new climate and socio-economic scenarios
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Constraints and potentials of future irrigation water availability on agricultural production under climate change
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Assessing agricultural risks of climate change in the 21st century in a global gridded crop model intercomparison
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2014
Cherian R., Quaas J., et al.
Pollution trends over Europe constrain global aerosol forcing as simulated by climate models
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2014
Zomer R. J., Trabucco A., et al.
Environmental stratification to model climate change impacts on biodiversity and rubber production in Xishuangbanna, Yunnan, China.
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Model%u2013data comparison and data assimilation of mid-Holocene Arctic sea ice concentration
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2014
Exbrayat J., Pitman A., et al.
Response of microbial decomposition to spin-up explains CMIP5 soil carbon range until 2100
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2014
Exbrayat J. -., Pitman A. J., et al.
Response of microbial decomposition to spin-up explains CMIP5 soil carbon range until 2100
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2014
Exbrayat J. F., Pitman A. J., et al.
Disentangling residence time and temperature sensitivity of microbial decomposition in a global soil carbon model
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2014
Grise K. M., Polvani L. M.
Is climate sensitivity related to dynamical sensitivity? A Southern Hemisphere perspective
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Statistical parameterization expressing ENSO variability and reversibility in response to CO2 concentration changes
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2014
Hartmann D. L., Ceppi P.
Trends in the CERES data set 2000-2013: The effects of ice melt and jet shifts and comparison to climate models
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2014
Steiner N. S., Christian J. R., et al.
Future ocean acidification in the Canada Basin and surrounding Arctic Ocean from CMIP5 earth system models
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The role of global climate change in the extreme low summer Arctic sea ice extent in 2012 in %u201CExplaining Extreme Events of 2012 from a Climate Perspective
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2013
Brands S., Herrera S., et al.
How well do CMIP5 Earth System Models simulate present climate conditions in Europe and Africa? A performance comparison for the downscaling community
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2013
Cattiaux J., Douville H., et al.
European temperatures in CMIP5: origins of present-day biases and future uncertainties
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2013
Cattiaux J., Cassou C.
Opposite CMIP3/5 trends in the Northern Annular Mode explained by combined local sea-ice and remote tropical influences
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2013
Davie J. C., Falloon P. D., et al.
Comparing projections of future changes in runoff from hydrological and biome models in ISI-MIP
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2013
Wilcox L. J., Charlton-Perez A. J.
Final warming of the Southern Hemisphere vortex in high- and low-top CMIP5 models
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2013
Wilcox L. J., Highwood E. J., et al.
The influence of anthropogenic aerosol on multi-decadal variations of historical global climate
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2013
Anav A., Friedlingstein P., et al.
EVALUATING THE LAND AND OCEAN COMPONENTS OF THE GLOBAL CARBON CYCLE IN THE CMIP5 EARTH SYSTEM MODELS
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A multi-model assessment of future projections of North Atlantic and European extratropical cyclones in the CMIP5 climate models
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