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Effect of water vapor on the determination of aerosol direct radiative effect based on the AERONET fluxes

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Academic year: 2017

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Figure 1. Radiative flux with aerosols F aer (plusses) and without aerosols F 0 (circles) as a function of AOD for the AERONET site in Kanpur in March–May and with SZA = 69 ◦ ± 1.5 ◦
Figure 2. Same as Fig. 1, but for the June–August season in (a) GSFC (SZA = 70 ◦ ), (b) Rio Branco (SZA = 70 ◦ ), (c) Dhadnah (SZA = 70 ◦ ), and (d) GSFC (SZA = 22 ◦ ).
Figure 3. ADRE predicted with exponential decay (a) and linear (b) regression methods (Eq
Table 1. The estimated ADRE (F aer ) with standard deviations compared with the AERONET value

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