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Hygroscopicity of atmospheric aerosol mostly is dependent upon the size and chemical structure of this particle and it is necessary for estimating anthropogenic aerosol radiative forcing. There is certainly limited information is present within the Indian region on size segregated aerosol hygroscopicity (κ) in various periods. This study presents 'κ' as derived from a Humidified Tandem Differential Mobility Analyzer (HTDMA) over a top Altitude Cloud Physics Laboratory (HACPL) in th
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