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Model calculations show that the aerosol particles within the lower troposphere usually contribute more than 80% to the total optical thickness of all particles within the atmosphere. For relative humidities higher than 99% within a thin layer of about 80 m thickness, the main contribution to the total optical thickness comes from this layer.
Model calculations show that the aerosol particles within the lower troposphere usually contribute more than 80% to the total optical thickness of all particles within the atmosphere. For relative humidities higher than 99% within a thin layer of about 80 m thickness, the main contribution to the total optical thickness comes from this layer.
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