Volcanoes and climate: Krakatoa's signature persists in the oceanClimatology: threatened loss of the Greenland ice-sheetPenetration of human-induced warming into the world's oceans.The inconstancy of the transient climate response parameter under increasing CO2.The effects of climate change on storm surges around the United Kingdom.A large ozone-circulation feedback and its implications for global warming assessments.Ice-sheet contributions to future sea-level change.Ice Sheet Model Intercomparison Project (ISMIP6) contribution to CMIP6.Sea-level rise by 2100.Revisiting the Earth's sea-level and energy budgets from 1961 to 2008Calibrated prediction of Pine Island Glacier retreat during the 21st and 22nd centuries with a coupled flowline modelModelling Antarctic and Greenland volume changes during the 20th and 21st centuries forced by GCM time slice integrationsEnergy budget constraints on climate responseCorrection to “Revisiting the Earth's sea-level and energy budgets from 1961 to 2008”Evaluating the ability of process based models to project sea-level changeThe impact of natural and anthropogenic forcings on climate and hydrology since 1550Studies of intermediate vector boson production and decay in UA1 at the CERN proton-antiproton colliderTwo-jet mass distributions at the CERN proton-antiproton colliderProduction of low transverse energy clusters in collisions at √s=0.2–0.9 TeV and their interpretation in terms of QCD jetsThe Flux-Anomaly-Forced Model Intercomparison Project (FAFMIP) contribution to CMIP6: investigation of sea-level and ocean climate change in response to CO2 forcingSystematic optimisation and climate simulation of FAMOUS, a fast version of HadCM3What Climate Sensitivity Index Is Most Useful for Projections?A data model of the Climate and Forecast metadata conventions (CF-1.6) with a software implementation (cf-python v2.1)A CF data model and implementationA traceable physical calibration of the vertical advection-diffusion equation for modeling ocean heat uptakeThe last glacial cycle: transient simulations with an AOGCMUnderstanding and Projecting Sea Level ChangeUnderstanding processes contributing to regional sea level changeDependence of the land-sea contrast in surface climate response on the nature of the forcingTropospheric Adjustment Induces a Cloud Component in CO2ForcingA new feedback on climate change from the hydrological cycleThe UA1 upgrade calorimeter trigger processorFast two dimensional cluster finding in particle physicsThe new UA1 calorimeter trigger processorUA1 upgrade first-level calorimeter trigger processor
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description
British climate modeller; Prof ...... e in the University of Reading
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Jonathan M. Gregory
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Jonathan M. Gregory
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Jonathan M. Gregory
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Jonathan M. Gregory
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Jonathan Gregory
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Jonathan Michael Gregory
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Jonathan M. Gregory
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Jonathan M. Gregory
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Jonathan M. Gregory
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Jonathan M. Gregory
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