about
Contribution of Arctic seabird-colony ammonia to atmospheric particles and cloud-albedo radiative effect.Large contribution of natural aerosols to uncertainty in indirect forcing.Mass spectra deconvolution of low, medium, and high volatility biogenic secondary organic aerosol.Assessing the influence of secondary organic versus primary carbonaceous aerosols on long-range atmospheric polycyclic aromatic hydrocarbon transport.Organic aerosol formation from photochemical oxidation of diesel exhaust in a smog chamber.Rethinking organic aerosols: semivolatile emissions and photochemical aging.Impact of gas-to-particle partitioning approaches on the simulated radiative effects of biogenic secondary organic aerosolA simple model of global aerosol indirect effectsThe magnitude and causes of uncertainty in global model simulations of cloud condensation nucleiCan cosmic rays affect cloud condensation nuclei by altering new particle formation rates?Cosmic rays, aerosol formation and cloud-condensation nuclei: sensitivities to model uncertaintiesCorrigendum to "The magnitude and causes of uncertainty in global model simulations of cloud condensation nuclei" published in Atmos. Chem. Phys., 13, 8879–8914, 2013Cosmic rays, aerosols, clouds, and climate: Recent findings from the CLOUD experimentAerosol size distribution and radiative forcing response to anthropogenically driven historical changes in biogenic secondary organic aerosol formationReduced efficacy of marine cloud brightening geoengineering due to in-plume aerosol coagulation: parameterization and global implicationsComparison of wildfire smoke estimation methods and associations with cardiopulmonary-related hospital admissionsIdentifying the sources driving observed PM<sub>2.5</sub> temporal variability over Halifax, Nova Scotia, during BORTAS-BFuture Fire Impacts on Smoke Concentrations, Visibility, and Health in the Contiguous United StatesEvaluation of observed and modelled aerosol lifetimes using radioactive tracers of opportunity and an ensemble of 19 global modelsThe importance of interstitial particle scavenging by cloud droplets in shaping the remote aerosol size distribution and global aerosol-climate effectsInterpreting aerosol lifetimes using the GEOS-Chem model and constraints from radionuclide measurementsSpatially and seasonally resolved estimate of the ratio of organic mass to organic carbonUncertainty associated with convective wet removal of entrained aerosols in a global climate modelBoundary layer new particle formation over East Antarctic sea ice – possible Hg-driven nucleation?Boundary layer new particle formation over East Antarctic sea ice – possible Hg driven nucleation?Organic condensation: a vital link connecting aerosol formation to cloud condensation nuclei (CCN) concentrationsQuantification of the volatility of secondary organic compounds in ultrafine particles during nucleation eventsInvestigation of particle and vapor wall-loss effects on controlled wood-smoke smog-chamber experimentsSoftware to analyze the relationship between aerosol, clouds, and precipitation: SAMACThe contribution of plume-scale nucleation to global and regional aerosol and CCN concentrations: evaluation and sensitivity to emissions changesA comparison of four receptor models used to quantify the boreal wildfire smoke contribution to surface PM<sub>2.5</sub> in Halifax, Nova Scotia during the BORTAS-B experimentAged boreal biomass-burning aerosol size distributions from BORTAS 2011Toward resolution-independent dust emissions in global models: Impacts on the seasonal and spatial distribution of dustWeak global sensitivity of cloud condensation nuclei and the aerosol indirect effect to Criegee + SO<sub>2</sub> chemistryFormation and growth of nucleated particles into cloud condensation nuclei: model–measurement comparisonSemi-empirical parameterization of size-dependent atmospheric nanoparticle growth in continental environmentsQuantifying the impact of BOReal forest fires on Tropospheric oxidants over the Atlantic using Aircraft and Satellites (BORTAS) experiment: design, execution and science overviewA Computationally Efficient Aerosol Nucleation/ Condensation Method: Pseudo-Steady-State Sulfuric AcidAnalysis of feedbacks between nucleation rate, survival probability and cloud condensation nuclei formationRepresentation of nucleation mode microphysics in a global aerosol model with sectional microphysics
P50
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P50
description
American atmospheric scientist
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atmosfeerwetenschapper
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name
Jeffrey R Pierce
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Jeffrey R Pierce
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Jeffrey R. Pierce
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Jeffrey R. Pierce
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Jeffrey R. Pierce
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Jeffrey R. Pierce
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Jeffrey R. Pierce
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Jeffrey R Pierce
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Jeffrey R Pierce
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Jeffrey R. Pierce
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Jeffrey R. Pierce
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Jeffrey R. Pierce
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Jeffrey R. Pierce
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Jeffrey R. Pierce
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J. R. Pierce
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Jeffrey Pierce
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Pierce JR
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Jeffrey R Pierce
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Jeffrey R Pierce
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Jeffrey R. Pierce
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Jeffrey R. Pierce
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Jeffrey R. Pierce
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Jeffrey R. Pierce
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Jeffrey R. Pierce
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P108
P1053
E-4681-2013
P1960
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P2038
Jeffrey_Pierce5
P21
P31
P3829
P496
0000-0002-4241-838X