New particle formation of liquid or solid nanoparticles from gas-phase precursors is a
decisive process in Earth's atmosphere and is considered one of the largest uncertainties in …

Brown carbon (BrC) has been recognized as an important contributor to global warming due
to its absorption of solar radiation with strong wavelength dependence. While early studies …

Short‑lived climate forcers (SLCFs) affect climate and are, in most cases, also air pollutants.
They include aerosols (sulphate, nitrate, ammonium, carbonaceous aerosols, mineral dust …

Anthropogenic secondary organic aerosol (ASOA), formed from anthropogenic emissions of
organic compounds, constitutes a substantial fraction of the mass of submicron aerosol in …

Satellite-based retrievals of tropospheric NO 2 columns are widely used to infer NO x (≡
NO+ NO 2) emissions. These retrievals rely on model information for the vertical distribution …

Abstract The Community Earth System Model version 2 (CESM2) includes three main
atmospheric configurations: the Community Atmosphere Model version 6 (CAM6) with …

The impact of aerosols on human health and climate is well-recognized, yet many studies
have only focused on total PM2. 5 or changes from anthropogenic activities. This study …

Atmospheric ice nucleating particles (INPs) influence global climate by altering cloud
formation, lifetime, and precipitation efficiency. The role of secondary organic aerosol (SOA) …

Submicron aerosol (PM1) species measured by aerosol mass spectrometers have been
widely used to validate chemical transport models; however, the uncertainties due to …

Reactive trace gas emissions from the polar oceans are poorly characterized, even though
their effects on atmospheric chemistry and aerosol formation are crucial for assessing …