14 citations as recorded by crossref.

1. Arctic marine secondary organic aerosol contributes significantly to summertime particle size distributions in the Canadian Arctic Archipelago B. Croft et al. 10.5194/acp-19-2787-2019
2. Characterizing the hygroscopicity of growing particles in the Canadian Arctic summer R. Chang et al. 10.5194/acp-22-8059-2022
3. Highly Hygroscopic Aerosols Facilitate Summer and Early‐Autumn Cloud Formation at Extremely Low Concentrations Over the Central Arctic Ocean P. Duplessis et al. 10.1029/2023JD039159
4. Impact of Biomass Burning on Arctic Aerosol Composition Y. Gramlich et al. 10.1021/acsearthspacechem.3c00187
5. Large Summer Contribution of Organic Biogenic Aerosols to Arctic Cloud Condensation Nuclei R. Lange et al. 10.1029/2019GL084142
6. Hygroscopicity and CCN Activity of Water‐Soluble Extracts From the Arctic Aerosols in Winter to Early Summer K. Kawana et al. 10.1029/2021JD035979
7. Aerosol and dynamical contributions to cloud droplet formation in Arctic low-level clouds G. Motos et al. 10.5194/acp-23-13941-2023
8. Measurement report: High Arctic aerosol hygroscopicity at sub- and supersaturated conditions during spring and summer A. Massling et al. 10.5194/acp-23-4931-2023
9. A long-term study of cloud residuals from low-level Arctic clouds L. Karlsson et al. 10.5194/acp-21-8933-2021
10. Size‐resolved measurements of mixing state and cloud‐nucleating ability of aerosols in Nanjing, China Y. Ma et al. 10.1002/2017JD026583
11. Indirect Measurements of the Composition of Ultrafine Particles in the Arctic Late‐Winter D. Myers et al. 10.1029/2021JD035428
12. Using Novel Molecular-Level Chemical Composition Observations of High Arctic Organic Aerosol for Predictions of Cloud Condensation Nuclei K. Siegel et al. 10.1021/acs.est.2c02162
13. Size‐dependent hygroscopicity parameter (κ) and chemical composition of secondary organic cloud condensation nuclei D. Zhao et al. 10.1002/2015GL066497
14. The seasonal characteristics of cloud condensation nuclei (CCN) in the arctic lower troposphere C. Jung et al. 10.1080/16000889.2018.1513291