Formation and cycling of aerosols in the global troposphere
暂无分享,去创建一个
John H. Seinfeld | Elisabetta Vignati | Jean-Philippe Putaud | J. Seinfeld | P. Adams | E. Vignati | J. Putaud | R. Dingenen | F. Raes | Frank Raes | Julian Wilson | Rita Van Dingenen | P. J. Adams | Julian Wilson
[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 .
[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.