Abstract
The paper investigates about the aerosol index (AI) parameter obtained from the OMI during 2002–2016 concluded an East China, which have been discovered with a strong spatial heterogeneity in AI over the East China indicates variety of sources. We observed significant change in spatial AI increasing from the South to North attributed to impact for the powder unit’s ecstatic since Recompense sections. Spatial relative tendencies showed that the AI is the highest in most provinces. Further, the short-wave cloud radiative forcing (SWCRF) distribution revealed the highest (−180 Wm−2) and lowest (−110 Wm−2) values during JJA and DJF, respectively. While the long-wave CRF (LWCRF) values were seen prominent in almost the entire study area, with the high (60 W m−2) in JJA and low during MAM over the southeastern sites of study domain.
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