资源环境科技发展态势分析平台

New particle formation (NPF) and growth can be an important source of cloud condensation nuclei (CCN) for the Arctic atmosphere, where cloud formation is sensitive to their availability. Low-level clouds influence the Arctic energy budget, and likely contribute to amplified Arctic warming. Molecular information of NPF is rarely reported, despite its importance to determine sources of condensing vapors and nucleation mechanisms. Beck et al. (2020) shed light on the complexity of NPF and growth at two Arctic locations. They reveal that chemical drivers and sources, are diverse across the Arctic. This advance in knowledge calls for similar studies throughout all seasons and in various Arctic environments to obtain a more systematic understanding of NPF and growth.