The global heat budget is a balance between incoming and outgoingsolarradiation.
The earth only receives 50% of the sun’senergy.
When the sun’s energy reaches the earth’s atmosphere, some is reflected and absorbed.
The lighter and brighter the cloud, the more insolation it will reflect.
The larger and darker the cloud, the more insolation it will absorb.
This is due to the albedo which is the rate of reflection.
The earth has areas with lots of ice and snow. These areas have a highalbedo, a high rate of reflection.
The earth has dark dense areas of vegetation such as the rainforest and there are vast oceans. These areas have a low albedo, a low rate of reflection.
Sulphur is emitted into the atmosphere by volcanoes. This will reflect the suns’ energy.
Pollution caused by humans emits CO2 and methane into the atmosphere. This gas will reflect the sun’s energy.