about
sameAs
Results from the CERN pilot CLOUD experimentBoreal forests, aerosols and the impacts on clouds and climateOn the relationship between aerosol model uncertainty and radiative forcing uncertaintyOccurrence of pristine aerosol environments on a polluted planetUnderstanding the nature of atmospheric acid processing of mineral dusts in supplying bioavailable phosphorus to the oceansImproving our fundamental understanding of the role of aerosol-cloud interactions in the climate system.The magnitude and sources of uncertainty in global aerosol.Ion-induced nucleation of pure biogenic particles.Reduced anthropogenic aerosol radiative forcing caused by biogenic new particle formation.Evidence for the role of organics in aerosol particle formation under atmospheric conditions.Cosmic rays, clouds, and climate.Excess mortality in Europe following a future Laki-style Icelandic eruptionNew approaches to quantifying aerosol influence on the cloud radiative effect.Collocated observations of cloud condensation nuclei, particle size distributions, and chemical composition.Strong constraints on aerosol-cloud interactions from volcanic eruptions.The role of low-volatility organic compounds in initial particle growth in the atmosphere.The detection of large HNO3-containing particles in the winter Arctic stratosphere.Arctic ozone loss due to denitrificationLarge contribution of natural aerosols to uncertainty in indirect forcing.Impact on short-lived climate forcers increases projected warming due to deforestation.Strong control of Southern Ocean cloud reflectivity by ice-nucleating particles.Impact on short-lived climate forcers (SLCFs) from a realistic land-use change scenario via changes in biogenic emissions.A marine biogenic source of atmospheric ice-nucleating particles.The importance of feldspar for ice nucleation by mineral dust in mixed-phase clouds.Atmospheric physics: Cosmic rays, clouds and climate.Minor effect of physical size sorting on iron solubility of transported mineral dustEvaluating uncertainty in convective cloud microphysics using statistical emulationExperimental investigation of ion–ion recombination under atmospheric conditionsImpact of gas-to-particle partitioning approaches on the simulated radiative effects of biogenic secondary organic aerosolModelled and observed changes in aerosols and surface solar radiation over Europe between 1960 and 2009Particulate matter, air quality and climate: lessons learned and future needsQuantifying sources of inter-model diversity in the cloud albedo effectAerosol microphysics simulations of the Mt.~Pinatubo eruption with the UM-UKCA composition-climate modelAn AeroCom assessment of black carbon in Arctic snow and sea iceIntercomparison and evaluation of global aerosol microphysical properties among AeroCom models of a range of complexityThe AeroCom evaluation and intercomparison of organic aerosol in global modelsThe complex response of Arctic aerosol to sea-ice retreatThe direct and indirect radiative effects of biogenic secondary organic aerosolUncertainty in the magnitude of aerosol-cloud radiative forcing over recent decadesBoundary layer nucleation as a source of new CCN in savannah environment
P50
Modelling the effects of realistic polar stratospheric clouds on past climate and future ozoneGlobal Modelling of Aerosols and Chemistry in Support of SOLAS-UKThe effects of particle formation on global aerosol and climateProcess analysis, observations and modelling - Integrated solutions for cleaner air for Delhi (PROMOTE)
P710
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P50
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P1344
P1053
C-8514-2009
P106
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P2002
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P2038
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P2070
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P21
P31
P3829
P496
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