31 citations as recorded by crossref.

1. The potential role of methanesulfonic acid (MSA) in aerosol formation and growth and the associated radiative forcings A. Hodshire et al.
2. J-GAIN v1.1: a flexible tool to incorporate aerosol formation rates obtained by molecular models into large-scale models D. Yazgi & T. Olenius
3. The importance of interstitial particle scavenging by cloud droplets in shaping the remote aerosol size distribution and global aerosol-climate effects J. Pierce et al.
4. Implementing a sectional scheme for early aerosol growth from new particle formation in the Norwegian Earth System Model v2: comparison to observations and climate impacts S. Blichner et al.
5. A sulfuric acid nucleation potential model for the atmosphere J. Johnson & C. Jen
6. Current state of aerosol nucleation parameterizations for air-quality and climate modeling K. Semeniuk & A. Dastoor
7. Reassessing the relative role of anthropogenic aerosols and natural decadal variability in driving the mid-twentieth century global “cooling”: a focus on the latitudinal gradient of tropospheric temperature C. Diao & Y. Xu
8. Vertical profiles of light absorption and scattering associated with black carbon particle fractions in the springtime Arctic above 79° N W. Leaitch et al.
9. Simulating the radiative forcing of oceanic dimethylsulfide (DMS) in Asia based on machine learning estimates J. Zhao et al.
10. Improved estimates of preindustrial biomass burning reduce the magnitude of aerosol climate forcing in the Southern Hemisphere P. Liu et al.
11. Reduced effective radiative forcing from cloud–aerosol interactions (ERFaci) with improved treatment of early aerosol growth in an Earth system model S. Blichner et al.
12. Modeling the Formation of Organic Compounds across Full Volatility Ranges and Their Contribution to Nanoparticle Growth in a Polluted Atmosphere Z. Li et al.
13. Ambient Particulate Matter Size Distributions Drive Regional and Global Variability in Particle Deposition in the Respiratory Tract J. Kodros et al.
14. Molecular-resolution simulations of new particle formation: Evaluation of common assumptions made in describing nucleation in aerosol dynamics models T. Olenius & I. Riipinen
15. The contribution of coral-reef-derived dimethyl sulfide to aerosol burden over the Great Barrier Reef: a modelling study S. Fiddes et al.
16. Atmospheric nanoparticle growth D. Stolzenburg et al.
17. Size-resolved mixing state of black carbon in the Canadian high Arctic and implications for simulated direct radiative effect J. Kodros et al.
18. Analysis of feedbacks between nucleation rate, survival probability and cloud condensation nuclei formation D. Westervelt et al.
19. New Parameterizations for Neutral and Ion‐Induced Sulfuric Acid‐Water Particle Formation in Nucleation and Kinetic Regimes A. Määttänen et al.
20. Modeling particle nucleation and growth over northern California during the 2010 CARES campaign A. Lupascu et al.
21. Contribution of expanded marine sulfur chemistry to the seasonal variability of dimethyl sulfide oxidation products and size-resolved sulfate aerosol L. Tashmim et al.
22. Particle Size as a Key Driver of Black Carbon Wet Removal: Advances and Insights Y. Qiao et al.
23. Uncertainties in global aerosols and climate effects due to biofuel emissions J. Kodros et al.
24. Machine Learning to Predict the Global Distribution of Aerosol Mixing State Metrics M. Hughes et al.
25. Factors controlling marine aerosol size distributions and their climate effects over the northwest Atlantic Ocean region B. Croft et al.
26. Processes controlling the annual cycle of Arctic aerosol number and size distributions B. Croft et al.
27. Evaluation of the global aerosol microphysical ModelE2-TOMAS model against satellite and ground-based observations Y. Lee et al.
28. The aerosol radiative effects of uncontrolled combustion of domestic waste J. Kodros et al.
29. New Particle Formation in the Atmosphere: From Molecular Clusters to Global Climate S. Lee et al.
30. Changes in global DMS production driven by increased CO2 levels and its impact on radiative forcing J. Zhao et al.
31. Extrapolating particle concentration along the size axis in the nanometer size range requires discrete rate equations T. Olenius et al.