Earth's net radiation, sometimes referred to as net flux, is the balance between incoming and outgoing solar radiation energy from the atmosphere. This study utilised five years of data on tropospheric variables (solar radiation, air temperature, surface temperature, maximum temperature, minimum temperature, and dew point temperature), from January 2007 to December 2011 to estimate net radiation and examine its temporal (diurnal) and daily variation. The measurement site is the old site of the Nigerian Television Authority, NTA Akure at Iju (7.15oN, 5.12oE), in Akure North Local Government area of Ondo State. The results indicate that the net radiation exhibits a radiant energy surplus during the daytime and a deficit at nighttime. The daily mean maximum of the hourly net radiation flux was about 550 Wm-2 for the dry season. The value occurred around 12:00 hrs and 380 Wm-2 for the wet season, the value occurring around 12:30 hrs. We observed a time lag between net radiation and temperature; the net radiative flux reached its maximum at 12:00 hrs while the temperature attained its peak value around 15:00 hrs. Daily averages of net radiation exhibited dual peaks with values of about 160 Wm-2day-1 around February and November and a minimum of about 50 Wm-2day-1. The daily average temperature has a singular peak in February, the hottest month. We also analysed daily net radiation values from 10 models that differ in structure and complexity, and a lot of them underestimated the standard model because they were location-dependent.
Olabintan et al. (Mon,) studied this question.