Formation and cycling of aerosols in the global troposphere

[1]  H. Maring,et al.  Aerosol physical and optical properties and their relationship to aerosol composition in the free troposphere at Izaña, Tenerife, Canary Islands, during July 1995 , 2000 .

[2]  J. Brenguier,et al.  Microphysical properties of stratocumulus clouds during ACE‐2 , 2000 .

[3]  J. Seinfeld,et al.  CCN measurements during ACE-2 and their relationship to cloud microphysical properties , 2000 .

[4]  L. Pirjola,et al.  Stable sulphate clusters as a source of new atmospheric particles , 2000, Nature.

[5]  Dimitrios Kotzias,et al.  Carboxylic Acids in Secondary Aerosols from Oxidation of Cyclic Monoterpenes by Ozone , 2000 .

[6]  R. Dingenen,et al.  Size distribution and chemical composition of marine aerosols: a compilation and review , 2000 .

[7]  D. Covert,et al.  Hygroscopic properties of aerosol particles in the north-eastern Atlantic during ACE-2 , 2000 .

[8]  K. Noone,et al.  Vertical profiles of aerosol scattering and absorption measured in situ during the North Atlantic Aerosol Characterization Experiment (ACE-2) , 2000 .

[9]  R. Van Dingenen,et al.  A simple non-linear analytical relationship between aerosol accumulation number and sub-micron volume, explaining their observed ratio in the clean and polluted marine boundary layer , 2000 .

[10]  Steven Businger,et al.  An overview of the Lagrangian experiments undertaken during the North Atlantic regional Aerosol Characterisation Experiment (ACE-2) , 2000 .

[11]  R. Van Dingenen,et al.  Chemical mass closure and assessment of the origin of the submicron aerosol in the marine boundary layer and the free troposphere at Tenerife during ACE-2 , 2000 .

[12]  J. Seinfeld,et al.  A comparative review of inorganic aerosol thermodynamic equilibrium modules: similarities, differences, and their likely causes , 2000 .

[13]  J. Seinfeld,et al.  Ternary nucleation of H2SO4, NH3, and H2O in the atmosphere , 1999 .

[14]  M. Chin,et al.  Tropospheric sulfur simulation and sulfate direct radiative forcing in the Goddard Institute for Space Studies general circulation model , 1999 .

[15]  D. Rosenfeld TRMM observed first direct evidence of smoke from forest fires inhibiting rainfall , 1999 .

[16]  John H. Seinfeld,et al.  Gas-Phase Ozone Oxidation of Monoterpenes: Gaseous and Particulate Products , 1999 .

[17]  M. Facchini,et al.  Cloud albedo enhancement by surface-active organic solutes in growing droplets , 1999, Nature.

[18]  Donald Dabdub,et al.  Estimate of global atmospheric organic aerosol from oxidation of biogenic hydrocarbons , 1999 .

[19]  P. Mcmurry,et al.  Particle production near marine clouds: Sulfuric acid and predictions from classical binary nucleation , 1999 .

[20]  John H. Seinfeld,et al.  Global concentrations of tropospheric sulfate, nitrate, and ammonium aerosol simulated in a general circulation model , 1999 .

[21]  J. Putaud,et al.  Processes determining the relationship between aerosol number and non‐sea‐salt sulfate mass concentrations in the clean and perturbed marine boundary layer , 1999 .

[22]  J. Seinfeld,et al.  A study of processes that govern the maintenance of aerosols in the marine boundary layer , 1999 .

[23]  John Y. N. Cho,et al.  Ubiquity of quasi-horizontal layers in the troposphere , 1999, Nature.

[24]  P. Kasibhatla,et al.  Is aerosol production within the remote marine boundary layer sufficient to maintain observed concentrations , 1999 .

[25]  John H. Seinfeld,et al.  Organic aerosol formation from the oxidation of biogenic hydrocarbons , 1999 .

[26]  R. Dingenen,et al.  Hygroscopic properties of aerosol formed by oxidation of limonene, α‐pinene, and β‐pinene , 1999 .

[27]  Mahoney,et al.  In situ measurements of organics, meteoritic material, mercury, and other elements in aerosols at 5 to 19 kilometers , 1998, Science.

[28]  Bandy,et al.  Particle nucleation in the tropical boundary layer and its coupling to marine sulfur sources , 1998, Science.

[29]  C. Sprengard-Eichel,et al.  Soluble and insoluble fractions of urban, continental and marine aerosol , 1998 .

[30]  U. Baltensperger,et al.  Heterogeneous production of nitrous acid on soot in polluted air masses , 1998, Nature.

[31]  P. Mcmurry,et al.  Rapid growth of freshly formed nanoparticles in the remote troposphere , 1998 .

[32]  R. Balling,et al.  Weekly cycles of air pollutants, precipitation and tropical cyclones in the coastal NW Atlantic region , 1998, Nature.

[33]  Antony D. Clarke,et al.  Particle production in the remote marine atmosphere: Cloud outflow and subsidence during ACE 1 , 1998 .

[34]  P. Quinn,et al.  Processes controlling the distribution of aerosol particles in the lower marine boundary layer during the First Aerosol Characterization Experiment (ACE 1) , 1998 .

[35]  D. Rind,et al.  An empirical model study of the tropospheric meridional circulation based on SAGE II observations , 1998 .

[36]  M. Schulz,et al.  Role of aerosol size distribution and source location in a three‐dimensional simulation of a Saharan dust episode tested against satellite‐derived optical thickness , 1998 .

[37]  M. Rood,et al.  Influence of Soluble Surfactant Properties on the Activation of Aerosol Particles Containing Inorganic Solute , 1998 .

[38]  Dimitrios Kotzias,et al.  cis-Pinic acid, a possible precursor for organic aerosol formation from ozonolysis of α-pinene , 1998 .

[39]  L. Pirjola,et al.  Parameterizations for sulfuric acid/water nucleation rates , 1998 .

[40]  S. Kreidenweis,et al.  Influence of sea-salt on aerosol radiative properties in the Southern Ocean marine boundary layer , 1998, Nature.

[41]  R. Turco,et al.  A new source of tropospheric aerosols: Ion‐ion recombination , 1998 .

[42]  Markku Kulmala,et al.  The potential for atmospheric mixing processes to enhance the binary nucleation rate , 1998 .

[43]  J. Seinfeld,et al.  Atmospheric Chemistry and Physics: From Air Pollution to Climate Change , 1998 .

[44]  P. Hobbs,et al.  Airborne measurements of carbonaceous aerosols on the East Coast of the United States , 1997 .

[45]  B. Anderson,et al.  Atmospheric layers measured from the NASA DC-8 during PEM-West B and comparison with PEM-West A , 1997 .

[46]  D. Blake,et al.  Vertical transport of sulfur dioxide and dimethyl sulfide in deep convection and its role in new particle formation , 1997 .

[47]  B. Anderson,et al.  Gas‐to‐particle conversion of tropospheric sulfur as estimated from observations in the western North Pacific during PEM‐West B , 1997 .

[48]  S. Madronich,et al.  New insights on OH: Measurements around and in clouds , 1997 .

[49]  Mian Chin,et al.  Contribution of different aerosol species to the global aerosol extinction optical thickness: Estimates from model results , 1997 .

[50]  P. V. Velthoven,et al.  Observations of aerosols in the free troposphere and marine boundary layer of the subtropical Northeast Atlantic: Discussion of processes determining their size distribution , 1997 .

[51]  M. Kulmala,et al.  Clouds without supersaturation , 1997, Nature.

[52]  Jean-Pierre Blanchet,et al.  Modeling sea-salt aerosols in the atmosphere 1. Model development , 1997 .

[53]  T. Gerz,et al.  Dispersion of aircraft exhausts in the free atmosphere , 1996 .

[54]  D. Jacob,et al.  Origin of ozone and NOx in the tropical troposphere: A photochemical analysis of aircraft observations over the South Atlantic basin , 1996 .

[55]  P. Crutzen,et al.  A mechanism for halogen release from sea-salt aerosol in the remote marine boundary layer , 1996, Nature.

[56]  J. Penner,et al.  A global three‐dimensional model study of carbonaceous aerosols , 1996 .

[57]  J. Wilson,et al.  A global black carbon aerosol model , 1996 .

[58]  Mian Chin,et al.  Anthropogenic and natural contributions to tropospheric sulfate: A global model analysis , 1996 .

[59]  J. Seinfeld,et al.  Time scales to achieve atmospheric gas-aerosol equilibrium for volatile species , 1996 .

[60]  J. Seinfeld,et al.  Gas/Particle Partitioning and Secondary Organic Aerosol Yields , 1996 .

[61]  P. Saxena,et al.  Water-soluble organics in atmospheric particles: A critical review of the literature and application of thermodynamics to identify candidate compounds , 1996 .

[62]  P. Quinn,et al.  Physical properties of marine boundary layer aerosol particles of the mid-Pacific in relation to sources and meteorological transport , 1996 .

[63]  A. Clarke,et al.  Lagrangian evolution of an aerosol column during the Atlantic Stratocumulus Transition Experiment , 1996 .

[64]  P. Pilewskie,et al.  Vertical profiles, aerosol microphysics, and optical closure during the Atlantic Stratocumulus Transition Experiment: Measured and modeled column optical properties , 1996 .

[65]  R. Synovec,et al.  Dissolution behavior and surface tension effects of organic compounds in nucleating cloud droplets , 1996 .

[66]  W. Read,et al.  Walker circulation and tropical upper tropospheric water vapor , 1996 .

[67]  M3 a multi modal model for aerosol dynamics , 1996 .

[68]  P. Mcmurry,et al.  MEASURED ATMOSPHERIC NEW PARTICLE FORMATION RATES: IMPLICATIONS FOR NUCLEATION MECHANISMS , 1996 .

[69]  R. Van Dingenen,et al.  Evidence for anthropogenic impact on number concentration and sulfate content of cloud‐processed aerosol particles over the North Atlantic , 1995 .

[70]  J. Seinfeld,et al.  Organics alter hygroscopic behavior of atmospheric particles , 1995 .

[71]  P. Seibert,et al.  A study of an outstanding Saharan dust event at the high-alpine site Jungfraujoch, Switzerland , 1995 .

[72]  Comment on ``The relationship between DMS flux and CCN concentration in remote marine regions'' by S. N. Pandis, L. M. Russell, and J. H. Seinfeld , 1995 .

[73]  P. Crutzen,et al.  The role of a deep convective storm over the tropical Pacific Ocean in the redistribution of atmospheric chemical species , 1995 .

[74]  D. Hegg,et al.  A preliminary study of the effect of ammonia on particle nucleation in the marine boundary layer , 1995 .

[75]  F. Raes Entrainment of free tropospheric aerosols as a regulating mechanism for cloud condensation nuclei in the remote marine boundary layer , 1995 .

[76]  P. Hobbs,et al.  Further evidence for particle nucleation in clear air adjacent to marine cumulus clouds , 1994 .

[77]  J. Seinfeld,et al.  Aerosol production and growth in the marine boundary layer , 1994 .

[78]  J. Seinfeld,et al.  The relationship between DMS flux and CCN concentration in remote marine regions , 1994 .

[79]  H. Hansson,et al.  Hygroscopic growth of aerosol particles and its influence on nucleation scavenging in cloud: Experimental results from Kleiner Feldberg , 1994 .

[80]  J. W. Fitzgerald,et al.  Marine boundary layer measurements of new particle formation and the effects nonprecipitating clouds have on aerosol size distribution , 1994 .

[81]  Leonard K. Peters,et al.  Binary Homogeneous Nucleation: Temperature and Relative Humidity Fluctuations, Nonlinearity, and Aspects of New Particle Production in the Atmosphere , 1994 .

[82]  J. Lelieveld,et al.  Role of Deep Cloud Convection in the Ozone Budget of the Troposphere , 1994, Science.

[83]  Reinout Boers,et al.  Coherence between seasonal variation in satellite-derived cloud optical depth and boundary layer CCN concentrations at a mid-latitude Southern Hemisphere station , 1994 .

[84]  J. W. Fitzgerald,et al.  A Cloud Chamber Study of the Effect That Nonprecipitating Water Clouds Have on the Aerosol Size Distribution , 1994 .

[85]  A. Clarke Atmospheric nuclei in the Pacific midtroposphere: Their nature, concentration, and evolution , 1993 .

[86]  J. Penner,et al.  Large contribution of organic aerosols to cloud-condensation-nuclei concentrations , 1993, Nature.

[87]  S. Hering,et al.  Mixing characteristics and water content of submicron aerosols measured in Los Angeles and at the grand canyon , 1993 .

[88]  M. H. Smith,et al.  Physicochemical properties of aerosols over the northeast Atlantic: Evidence for wind‐speed‐related submicron sea‐salt aerosol production , 1993 .

[89]  R. Dingenen,et al.  Cloud Condensation Nuclei from Dimethyl Sulphide in the Natural Marine Boundary Layer: Remote VS. In-Situ Production , 1993 .

[90]  P. Quinn,et al.  New particle formation in the marine boundary layer , 1992 .

[91]  R. Dingenen,et al.  Modelling formation and growth of H2SO4-H2O aerosols: Uncertainty analysis and experimental evaluation , 1992 .

[92]  R. Dingenen,et al.  Simulations of condensation and cloud condensation nuclei from biogenic SO2 in the remote marine boundary layer , 1992 .

[93]  J. Heintzenberg,et al.  On the state of mixing of particles due to Brownian coagulation , 1992 .

[94]  D. Covert,et al.  Modeling a case of particle nucleation in the marine boundary layer , 1992 .

[95]  A. Clarke Atmospheric nuclei in the remote free-troposphere , 1992 .

[96]  D. A. Carter,et al.  Long-Term Mean Vertical Motion over the Tropical Pacific: Wind-Profiling Doppler Radar Measurements , 1991, Science.

[97]  T. Bates,et al.  Sulfur isotope measurements of submicrometer sulfate aerosol particles over the Pacific Ocean , 1991 .

[98]  Henning Rodhe,et al.  A global three-dimensional model of the tropospheric sulfur cycle , 1991 .

[99]  R. W. Gillett,et al.  Coherence between seasonal cycles of dimethyl sulphide, methanesulphonate and sulphate in marine air , 1991, Nature.

[100]  L. Radke,et al.  Particle production associated with marine clouds , 1990 .

[101]  D. Covert,et al.  On the distribution of physical and chemical particle properties in the atmospheric aerosol , 1990 .

[102]  J. W. Fitzgerald,et al.  Aerosol size distributions and optical properties found in the marine boundary layer over the Atlantic Ocean , 1990 .

[103]  M. Heimann,et al.  Modelling the long-range transport of 222Rn to subantarctic and antarctic areas , 1990 .

[104]  P. Crutzen,et al.  Parameterization of vertical tracer transport due to deep cumulus convection in a global transport model and its evaluation with 222Radon measurements , 1990 .

[105]  J. Seinfeld,et al.  The distribution of ammonium salts among a size and composition dispersed aerosol , 1990 .

[106]  J. Heintzenberg Fine particles in the global troposphere. A review , 1989 .

[107]  A. Jaecker-Voirol,et al.  Heteromolecular nucleation in the sulfuric acid-water system , 1989 .

[108]  A. Jaecker-Voirol,et al.  Binary homogeneous nucleation , 1988 .

[109]  S. Warren,et al.  Oceanic phytoplankton, atmospheric sulphur, cloud albedo and climate , 1987, Nature.

[110]  T. Bates,et al.  Regional and seasonal variations in the flux of oceanic dimethylsulfide to the atmosphere , 1987 .

[111]  M. Andreae,et al.  Vertical distribution of dimethylsulphide in the marine atmosphere , 1986, Nature.

[112]  G. M. Frick,et al.  Effect of nonprecipitating clouds on the aerosol size distribution in the marine boundary layer , 1986 .

[113]  R. Dingenen,et al.  The role of ion-induced aerosol formation in the lower atmosphere , 1986 .

[114]  S. Friedlander,et al.  A general correlation for deposition of suspended particles from turbulent gases to completely rough surfaces , 1985 .

[115]  P. Crutzen,et al.  Sulfur dioxide in remote oceanic air: Cloud transport of reactive precursors , 1984 .

[116]  A. Oort,et al.  Global atmospheric circulation statistics, 1958-1973 , 1994 .

[117]  R. Turco,et al.  An analysis of various nucleation mechanisms for sulfate particles in the stratosphere , 1982 .

[118]  A. H. Woodcock,et al.  THE PRODUCTION, CONCENTRATION, AND VERTICAL DISTRIBUTION OF THE SEA‐SALT AEROSOL * , 1980 .

[119]  J. Klett,et al.  Microphysics of Clouds and Precipitation , 1978, Nature.

[120]  R. Newell,et al.  Climate and the Ocean , 1979 .

[121]  K. T. Whitby THE PHYSICAL CHARACTERISTICS OF SULFUR AEROSOLS , 1978 .

[122]  F. S. Lai,et al.  The self-preserving particle size distribution for Brownian coagulation in the free-molecule regime , 1972 .

[123]  B. J. Mason,et al.  The physics of clouds , 1971 .

[124]  C. N. Davies,et al.  The Mechanics of Aerosols , 1964 .

[125]  F. Went Blue Hazes in the Atmosphere , 1960, Nature.

[126]  H. Köhler The nucleus in and the growth of hygroscopic droplets , 1936 .

[127]  J. Aítken,et al.  On the Number of Dust Particles in the Atmosphere , 1888, Nature.