LACIS - Literature
- Stratmann et al. (2004), J. Atmos. Oceanic Technol., 21, 876-887: Laboratory studies and numerical simulations of cloud droplet formation under realistic super-saturation conditions.
- Kiselev et al. (2005), Appl. Opt., 44(22), 4693-4701: White-light optical particle spectrometer for in situ measurement of condensational growth of aerosol particles.
- Wex et al. (2005), J. Geophys. Res., D21212, doi:10.1029/2004JD005507: Measured and modeled equilibrium sizes of NaCl and (NH4)2SO4 particles at relative humidities up to 99.1%.
- Wex et al. (2006), Atmos. Chem. Phys., 6, 4519-4527: Calibration of LACIS as a CCN detector and its use in measuring activation and hygroscopic growth of atmospheric aerosol particles.
- Voigtländer et al. (2007), J. Geophys. Res., 112, D20208, doi:10.1029/2007JD008604: Mass accomodation coefficient of water: a combined computational fluid dynamics and experimental data analysis.
- Wex et al. (2007a), Geophys. Res. Lett., 34, L02818, doi:10.1029/ 2006GL028260: Hygroscopic growth and measured and modeled critical super-saturations of an atmospheric HULIS sample.
- Wex et al. (2007b), Geophys. Res. Lett., 34, L17810, doi:10.1029/2007GL030185: Deliquescence and hygroscopic growth of succinic acid particles measured with LACIS.
- Niedermeier et al. (2008), Atmos. Chem. Phys., 8, 579-590: LACIS-measurements and parameterization of see-salt particle hygroscopic growth and activation.
- Wex et al. (2008a), J. Atmos. Sci., 65, 4004-4016, doi:10.1175/2008JAS2720.1: The Kelvin versus the Raoult term in the Köhler equation.
- Wex et al. (2008b), Environ. Res. Lett., 3, doi:10.1088/1748-9326/3/3/035004: The role of surface tension in connecting hygroscopic growth to activation for different particle types.
- Ziese et al. (2008), Atmos. Chem. Phys., 8, 1855-1866: Hygroscopic growth and activation of HULIS particles: Experimental data and a new iterative parameterization scheme for complex aerosol particles.
- Juranyi et al. (2009), Phys. Chem. Chem. Phys., 11, 36, 8091-8097, doi:10.1039/b904162a: Influence of gas-to-particle partitioning on the hygroscopic and droplet activation behaviour of alpha-pinene secondary organic aerosol.
- Petters et al. (2009), Atmos. Chem. Phys., 9, 3999-4009: Towards closing the gap between hygroscopic growth and activation for secondary oganic aerosol - Part 2: Theoretical approaches.
- Stratmann et al. (2009), Ernst Strüngmann Forum reports, Frankfurt, Germany: Laboratory cloud simulation: Capabilities and future directions.
- Wex et al. (2009), Atmos. Chem. Phys., 9, 3987-3997: Towards closing the gap between hygroscopic growth and activation for secondary oganic aerosol: Part 1 - Evidence from measurements.
- Henning et al. (2010), J. Geophys. Res., 115, D11206, doi:10.1029/2009JD012626: Soluble mass, hygroscopic growth and droplet activation during LExNo.
- Kiselev et al. (2010), J. Geophys. Res., 115, D11204, doi:10.1029/2009JD012635: Morphological characterization of soot aerosol during LExNo.
- Niedermeier et al. (2010), Atmos. Chem. Phys., 10, 3601–3614: Heterogeneous freezing of droplets with immersed mineral dust particles – measurements and parameterization.
- Poulain et al. (2010), Atmos. Chem. Phys., 10, 3775–3785: Towards closing the gap between hygroscopic growth and activation for secondary oganic aerosol - Part 3: Influence of the chemical composition on the hygroscopic properties and volatile fractions of aerosol.
- Snider et al. (2010), J. Geophys. Res., 115, D11205, doi:10.1029/2009JD012618: Intercomparison of CCN and hygroscopic fraction measurements from LExNo.
- Stratmann et al. (2010), J. Geophys. Res., 115, D11203, doi:10.1029/2009JD012628: Examination of laboratory-generated coated soot particles: An overview over the LExNo campaign.
- Sullivan et al. (2010), Atmos. Chem. Phys. Discuss., 10, submitted: Irreversible loss of ice nucleation active sites in mineral dust particles caused by sulphuric acid condensation.
- Wex et al. (2010a), Geophys. Res. Lett., 37, L10805, doi:10.1029/2010GL043337: Influence of the external mixing state of atmospheric aerosol on derived CCN number concentrations.
- Wex et al. (2010b), Advances in Meteorology, accepted: The influence of algal exudate on the hygroscopicity of sea spray particles.
