«There is nothing inherently wrong with defining aerosol changes to be a forcing, but it is practically impossible to accurately determine the aerosol forcing because it depends sensitively on the geographical and altitude distribution of aerosols, aerosol absorption, and aerosol cloud effects for each of
several aerosol compositions.
Aerosol changes between those climate states are appropriately included as a fast feedback, not only because aerosols respond rapidly to changing climate but also because there are multiple aerosol compositions, they have complex radiative properties and they affect clouds in several ways, thus making accurate knowledge of their glacial — interglacial changes inacce
Aerosol changes between those climate states are appropriately included as a fast feedback, not only because
aerosols respond rapidly to changing climate but also because there are multiple
aerosol compositions, they have complex radiative properties and they affect clouds in several ways, thus making accurate knowledge of their glacial — interglacial changes inacce
aerosol compositions, they have complex radiative properties and they affect clouds in
several ways, thus making accurate knowledge of their glacial — interglacial changes inaccessible.