Abstract

The present study investigates the spectral distribution of global, direct (E<sub>bλ</sub>) and diffuse (E<sub>bλ</sub>) irradiances over Delhi with the help of handheld Field Spectroradiometer in the year 2014 – 2015. Seasonal variation in the solar irradiances as well as the diffuse-to-direct ratio ( E<sub>dλ</sub>/E<sub>bλ</sub>]) was studied during three seasons (post-monsoon, winter and pre-monsoon) having different atmospheric conditions. Observations were carried out under clear sky days during day time when solar zenith angle is low in order to get maximum solar radiation. The ratio E<sub>dλ</sub>/E<sub>bλ</sub> is used as a function to measure the impact of aerosol load on incoming solar irradiance. NASA's Aqua satellite, MODIS (Moderate Resolution Imaging Spectroradiometer) AOD<sub>550</sub> data has been used to evaluate the relationship between aerosol load and ratio (E<sub>dλ</sub>/E<sub>bλ</sub>) on incoming solar radiation. A strong dependence of measured diffuse-to-direct irradiance ratio (E<sub>dλ</sub>/E<sub>bλ</sub>) on wavelength was observed. It was found to be decreasing exponentially with wavelength. Value of E<sub>dλ</sub>/E<sub>bλ</sub> was found to be maximum and minimum during Post-monsoon and Pre-monsoon seasons respectively. Also, the maximum values of E<sub>dλ</sub>/E<sub>bλ</sub> ratio were observed at the shorter wavelengths in all the studied seasons. The AOD<sub>550</sub> value was found to be maximum during postmonsoon followed by winter and Pre-monsoon seasons. Crop residue burning in addition to low wind speed was responsible for high aerosol load during the post-monsoon season where as inversion layer and calm wind conditions favored high aerosol load during winter season. A strong relation between the ratio E<sub>dλ</sub>/E<sub>bλ</sub> and AOD<sub>550</sub> is observed in all the studied seasons, indicating that high aerosol load was responsible for the attenuation of the incoming solar radiation in all the seasons

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