one part is absorbed in the ozone layer, another part is reflected by clouds and the surface of the earth, the major part is absorbed by the surface of the earth.

one part is absorbed by the atmosphere, almost all of the incoming radiation reaches the surface of the earth, where it is completely absorbed, leading to maximum temperatures at the around.

the major part remains in the stratosphere, where the ozone layer is an effective absorber of solar radiation, temperatures in the ozone layer are therefore similar to surface temperatures.

the major part is absorbed by atmospheric gases and clouds, the temperature rise in the affected layers leads to long wave terrestrial radiation.