(i) Global mean maximum supersaturation, fine-aerosol (iii) hygroscopicity, and (v) wet radius, as well as coarse-aerosol (vii) hygroscopicity and (ix) wet radius, as calculated by EMAC from the base case simulation at the altitude of 940 hPa. Absolute difference between the base case and nitrate-aerosol-free (NAF) sensitivity simulation in (ii) maximum supersaturation, fine-aerosol (iv) hygroscopicity, and (vi) wet radius, as well as coarse-aerosol (viii) hygroscopicity and (x) wet radius at the altitude of 940 hPa. Red indicates higher values calculated by the base case simulation in the presence of NO3- aerosols.

(i) Global mean maximum supersaturation, fine-aerosol (iii) hygroscopicity, and (v) wet radius, as well as coarse-aerosol (vii) hygroscopicity and (ix) wet radius, as calculated by EMAC from the base case simulation at the altitude of 940 hPa. Absolute difference between the base case and nitrate-aerosol-free (NAF) sensitivity simulation in (ii) maximum supersaturation, fine-aerosol (iv) hygroscopicity, and (vi) wet radius, as well as coarse-aerosol (viii) hygroscopicity and (x) wet radius at the altitude of 940 hPa. Red indicates higher values calculated by the base case simulation in the presence of NO3- aerosols.

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Nitrate (NO3-) aerosol is projected to increase dramatically in the coming decades and may become the dominant inorganic particle species. This is due to the continued strong decrease in SO2 emissions, which is not accompanied by a corresponding decrease in NOx and especially NH3 emissions. Thus, the radiative effect (RE) of NO3- aerosol may become...