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Effects of dust aerosols on tropospheric chemistry during a typical pre-monsoon season dust storm in northern India

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Table 1. The heterogeneous reactions and dry reactive uptake coe ffi cients (γ dry ) used in this study are shown
Table 2. Simulations designs used in this study and their purpose are shown.
Fig. 1. The relative humidity dependence of reactive uptake coe ffi cient (γ) for ozone, HNO 3 , OH, HO 2 , H 2 O 2 and SO 2 used in this study.
Fig. 2. Variations in observed and WRF-Chem simulated (No_Dust, Dust_JH_NoRH, Dust_J and Dust_JH) daily average ozone (top panel) and NO y (middle panel) at Nainital during 13–24 April 2010
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