Fig. 11

Contrast of the CCF of the band, observable with GIANO, as a function of altitude of aerosols, expressed as pressure of the cloud top. The shadowed area is spanned by the models when the temperature is varied between 1200 and 2300 K. A sharp decrease in the contrast of the CCF is caused by aerosols higher than a critical pressure. For solar water abundance, this threshold is located at about 10−3 bar (blue curve). For 0.1 times solar abundance, this threshold is located at about 10−2 bar (red curve), thus 10 times deeper in the atmosphere.
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