This document discusses concepts related to solar radiation received on Earth. It defines the solar constant as the amount of incoming solar radiation at the top of the atmosphere, which is approximately 1350 W/m2 for Earth. It explains that albedo is the fraction of sunlight reflected by a planet and Earth's albedo is about 0.3, reflecting 30% of incoming solar radiation. Net radiation is defined as the difference between absorbed and emitted radiation, and an example is provided where net radiation at the surface is calculated to be 380 W/m2.