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Fig. 2 . Aerosol type is identified by using γ ′ and δ v to the extent possible from among one of the six types. However, γ ′ and δ v are not sufficient to fully constrain the model selection. Surface type is used to exploit differences in aerosol classes over the oceans, deserts, and snow/tundra regions. Information about aerosol layer elevation is also utilized to determine aerosol type, because conditions that favor lifting mechanisms for dust and smoke are more likely than for other
Fig. 2 . Aerosol type is identified by using γ ′ and δ v to the extent possible from among one of the six types. However, γ ′ and δ v are not sufficient to fully constrain the model selection. Surface type is used to exploit differences in aerosol classes over the oceans, deserts, and snow/tundra regions. Information about aerosol layer elevation is also utilized to determine aerosol type, because conditions that favor lifting mechanisms for dust and smoke are more likely than for other
