Trans-Pacific dust transport: integrated analysis of NASA/CALIPSO and a global aerosol transport modelThe heterogeneous reaction of hydroxyl radicals with sub-micron squalane particles: a model system for understanding the oxidative aging of ambient aerosolsThe formation, properties and impact of secondary organic aerosol: current and emerging issuesThe relationship between aerosol and cloud drop number concentrations in a global aerosol microphysics modelThe radiative forcing potential of different climate geoengineering options

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Trans-Pacific dust transport: integrated analysis of NASA/CALIPSO and a global aerosol transport modelK. Eguchi, I. Uno, K. Yumimoto, T. Takemura, A. Shimizu, N. Sugimoto,
The heterogeneous reaction of hydroxyl radicals with sub-micron squalane particles: a model system for understanding the oxidative aging of ambient aerosolsJ. D. Smith, J. H. Kroll, C. D. Cappa, D. L. Che, C. L.
The formation, properties and impact of secondary organic aerosol: current and emerging issuesM. Hallquist, J. C. Wenger, U. Baltensperger, Y. Rudich, D. Simpson, M
The relationship between aerosol and cloud drop number concentrations in a global aerosol microphysics modelK. J. Pringle, K. S. Carslaw, D. V. Spracklen, G. M. Mann, a
The radiative forcing potential of different climate geoengineering optionsT. M. Lenton and N. E. Vaughan
The impact of MM5 and WRF meteorology over complex terrain on CHIMERE model calculationsA. de Meij, A. Gzella, P. Thunis, C. Cuvelier, B. Bessagnet, J. F
Transport and vertical structure of aerosols and water vapor over West Africa during the African monsoon dry seasonS.-W. Kim, P. Chazette, F. Dulac, J. Sanak, B. Johnson, and S.-C. Yoon
The time evolution of aerosol size distribution over the Mexico City plateauL. I. Kleinman, S. R. Springston, J. Wang, P. H. Daum, Y.-N.
Technical Note: In-situ quantification of aerosol sources and sinks over regional geographical scalesG. Buzorius
Towards closing the gap between hygroscopic growth and activation for secondary organic aerosol: Part 1 – Evidence from measurementsH. Wex, M. D. Petters, C. M. Carrico, E. Hallbauer, A. Massling,
Technical Note: Feasibility of CO2 profile retrieval from limb viewing solar occultation made by the ACE-FTS instrumentP. Y. Foucher, A. Chédin, G. Dufour, V. Capelle, C. D. Boone, and
Time-span and spatial-scale of regional new particle formation events over Finland and Southern SwedenT. Hussein, H. Junninen, P. Tunved, A. Kristensson, M. Dal Maso, I.&nb
The role of surfactants in K?hler theory reconsideredR. Sorjamaa, B. Svenningsson, T. Raatikainen, S. Henning, M. Bilde, and A.&
The part of the solar spectrum with the highest influence on the formation of SOA in the continental boundary layerM. Boy and M. Kulmala
Three years of routine Raman lidar measurements of tropospheric aerosols: Backscattering, extinction, and residual layer heightJ. Schneider and R. Eixmann
The adsorption of nitrogen oxides on crystalline iceT. Bartels, B. Eichler, P. Zimmermann, H. W. G?ggeler, and M. Ammann
The UV-visible absorption cross-sections of IONO2J. C. M?ssinger, D. M. Rowley, and R. A. Cox
The impact of multiphase reactions of NO2 with aromatics: a modelling approachN. Lahoutifard, M. Ammann, L. Gutzwiller, B. Ervens, and Ch. George
The flux of carbonyl sulfide and carbon disulfide between the atmosphere and a spruce forestX. Xu, H. G. Bingemer, and U. Schmidt
Tropospheric NO2 columns: a comparison between model and retrieved data from GOME measurementsA. Lauer, M. Dameris, A. Richter, and J. P. Burrows

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