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
Aerosol-cloud interactions contribute to a large portion of the spread in estimates of climate forcing, climate sensitivity and future projections. An important part of this uncertainty is how much new particle formation (NPF) contributes to cloud condensation nuclei (CCN) and, furthermore, how this changes with changes in anthropogenic emissions. Incorporating NPF and early growth in Earth system
