0000000000496262

AUTHOR

Graham Mann

showing 4 related works from this author

A multi-model assessment of the efficacy of sea spray geoengineering

2012

Abstract. Artificially increasing the albedo of marine clouds by the mechanical emission of sea spray aerosol has been proposed as a geoengineering technique to slow the warming caused by anthropogenic greenhouse gases. A previous global model study found that only modest increases and sometimes even decreases in cloud drop number (CDN) concentrations would result from plausible emission scenarios. Here we extend that work to examine the conditions under which decreases in CDN can occur, and use three independent global models to quantify maximum achievable CDN changes. We find that decreases in CDN can occur when at least three of the following conditions are met: the injected particle num…

business.industryEnvironmental engineeringEnvironmental scienceGeoengineeringbusinessSea spray
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A multi-model assessment of the impact of sea spray geoengineering on cloud droplet number

2012

Artificially increasing the albedo of marine boundary layer clouds by the mechanical emission of sea spray aerosol has been proposed as a geoengineering technique to slow the warming caused by anthropogenic greenhouse gases. A previous global model study (Korhonen et al., 2010) found that only modest increases (< 20%) and sometimes even decreases in cloud drop number (CDN) concentrations would result from emission scenarios calculated using a windspeed dependent geoengineering flux parameterisation. Here we extend that work to examine the conditions under which decreases in CDN can occur, and use three independent global models to quantify maximum achievable CDN changes. We find that dec…

Atmospheric ScienceMeteorologybusiness.industryCloud coverDrop (liquid)Atmospheric sciencesSea spraylcsh:QC1-999Aerosollcsh:Chemistrylcsh:QD1-999Greenhouse gasGeometric standard deviationEnvironmental scienceGeoengineeringParticle sizebusinesslcsh:Physics
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Intercomparison and evaluation of global aerosol microphysical properties among AeroCom models of a range of complexity

2014

Many of the next generation of global climate models will include aerosol schemes which explicitly simulate the microphysical processes that determine the particle size distribution. These models enable aerosol optical properties and cloud condensation nuclei (CCN) concentrations to be determined by fundamental aerosol processes, which should lead to a more physically based simulation of aerosol direct and indirect radiative forcings. This study examines the global variation in particle size distribution simulated by 12 global aerosol microphysics models to quantify model diversity and to identify any common biases against observations. Evaluation against size distribution measurements from…

Atmospheric Science010504 meteorology & atmospheric sciencesParticle numbergeneral-circulation modelmixing state010501 environmental sciencesEnvironmentclimate modelblack carbonAtmospheric sciences01 natural sciencesTropospherelcsh:ChemistryZeppelinobservatorietUrban Developmentddc:550Cloud condensation nucleiBuilt Environmentnumber size distributionsPhysics::Atmospheric and Oceanic Physics0105 earth and related environmental sciencesMicrophysicsparticle formationEarth / EnvironmentalCloud physicsatmospheric aerosolCAS - Climate Air and SustainabilityRadiative forcinglcsh:QC1-999Aerosolcloud condensation nucleimarine boundary-layerlcsh:QD1-99913. Climate actionClimatologyEnvironmental scienceClimate modelELSS - Earth Life and Social Sciencesoff-line modellcsh:Physics
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The AeroCom evaluation and intercomparison of organic aerosol in global models

2014

This paper evaluates the current status of global modeling of the organic aerosol (OA) in the troposphere and analyzes the differences between models as well as between models and observations. Thirty-one global chemistry transport models (CTMs) and general circulation models (GCMs) have participated in this intercomparison, in the framework of AeroCom phase II. The simulation of OA varies greatly between models in terms of the magnitude of primary emissions, secondary OA (SOA) formation, the number of OA species used (2 to 62), the complexity of OA parameterizations (gas-particle partitioning, chemical aging, multiphase chemistry, aerosol microphysics), and the OA physical, chemical and op…

Atmospheric Science010504 meteorology & atmospheric sciencesMeteorologyChemical transport modelFÍSICA ATMOSFÉRICA010501 environmental sciencesAtmospheric sciences01 natural scienceslcsh:ChemistryTropospherePARTICULATE MATTERCHEMICAL-TRANSPORT MODELmedicineMass concentration (chemistry)GENERAL-CIRCULATION MODEL0105 earth and related environmental sciences[PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph]ATMOSPHERIC AEROSOLEARTH SYSTEMCLIMATE MODELVOLATILITY BASIS-SETParticulatesSeasonalitymedicine.diseaselcsh:QC1-999CARBONACEOUS AEROSOLSAerosolDeposition (aerosol physics)lcsh:QD1-999MASS-SPECTROMETER13. Climate action[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/ClimatologyVOLATILITY BASIS-SET BIOMASS BURNING EMISSIONS CHEMICAL-TRANSPORT MODEL GENERAL-CIRCULATION MODEL CLIMATE MODEL CARBONACEOUS AEROSOLS MASS-SPECTROMETER EARTH SYSTEM ATMOSPHERIC AEROSOL PARTICULATE MATTEREnvironmental scienceClimate modelBIOMASS BURNING EMISSIONSlcsh:Physics
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