Ice formation by black carbon particles
暂无分享,去创建一个
S. Kreidenweis | D. Rogers | P. DeMott | Yalei Chen | D. E. Sherman | Y. Chen | David C. Rogers | D. Sherman
[1] K. Diehl,et al. A laboratory study of the effects of a kerosene-burner exhaust on ice nucleation and the evaporation rate of ice crystals , 1998 .
[2] N. A. Kakutkina,et al. Ice nucleation on soot particles , 1998 .
[3] K. Sassen,et al. Toward the theory of homogeneous nucleation and its parameterization for cloud models , 1998 .
[4] A. Petzold,et al. Elemental composition and morphology of ice-crystal residual particles in cirrus clouds and contrails , 1998 .
[5] B. Kärcher. Physicochemistry of aircraft‐generated liquid aerosols, soot, and ice particles: 1. Model description , 1998 .
[6] S. Kreidenweis,et al. Single particle analyses of ice nucleating aerosols in the upper troposphere and lower stratosphere , 1998 .
[7] S. Kreidenweis,et al. Measurements of ice nucleating aerosols during SUCCESS , 1998 .
[8] Bruce E. Anderson,et al. Ice nucleation processes in upper tropospheric wave‐clouds observed during SUCCESS , 1998 .
[9] Cynthia H. Twohy,et al. Electron microscope analysis of residual particles from aircraft contrails , 1998 .
[10] S. Kreidenweis,et al. The role of heterogeneous freezing nucleation in upper tropospheric clouds: Inferences from SUCCESS , 1998 .
[11] J. Ström,et al. Real-time measurement of absorbing material in contrail ice using a counterflow virtual impactor , 1998 .
[12] Richard C. Miake-Lye,et al. Environmental conditions required for contrail formation and persistence , 1998 .
[13] Peter Brimblecombe,et al. Thermodynamic Model of the System H+−NH4+−SO42-−NO3-−H2O at Tropospheric Temperatures , 1998 .
[14] Richard P. Turco,et al. Contrail formation and impacts on aerosol properties in aircraft plumes: Effects of fuel sulfur content , 1998 .
[15] D. Murphy,et al. On the Purity of Laboratory-Generated Sulfuric Acid Droplets and Ambient Particles Studied by Laser Mass Spectrometry , 1997 .
[16] S. Kreidenweis,et al. The susceptibility of ice formation in upper tropospheric clouds to insoluble aerosol components , 1997 .
[17] M. Baker,et al. Cloud Microphysics and Climate , 1997 .
[18] G. C. Tiao,et al. Analysis of long-term behavior of ultraviolet radiation measured by Robertson-Berger meters at 14 sites in the United States , 1997 .
[19] D. Golden,et al. Reactive uptake and hydration experiments on amorphous carbon treated with NO2, SO2, O3, HNO3, and H2SO4 , 1997 .
[20] The potential impact of soot particles from aircraft exhaust on cirrus clouds , 1997 .
[21] U. Schumann,et al. The Initial Composition of Jet Condensation Trails , 1996 .
[22] P. Sheridan,et al. Aerosol particles in the upper troposphere and lower stratosphere: Elemental composition and morphology of individual particles in northern midlatitudes , 1994 .
[23] W. T. Rawlins,et al. Observation of hydration of single, modified carbon aerosols , 1994 .
[24] P. Machetel,et al. Convection within the inner‐core and thermal implications , 1992 .
[25] K. Snetsinger,et al. Black carbon (soot) aerosol in the lower stratosphere and upper troposphere , 1992 .
[26] Philip D. Whitefield,et al. A field sampling of jet exhaust aerosols , 1992 .
[27] P. DeMott. An Exploratory Study of Ice Nucleation by Soot Aerosols , 1990 .
[28] D. Rogers. Development of a continuous flow thermal gradient diffusion chamber for ice nucleation studies , 1988 .