Greenhouse effect: Certain gases in the atmosphere trap heat from the sun, leading to a warmer temperature, and preventing excessive heat loss.
Albedo effect: The reflectivity of the Earth's surface affects how much sunlight is absorbed, with lighter surfaces reflecting more heat.
Cloud cover: Clouds can reflect solar radiation, cooling the surface, or trap heat radiating from the Earth, warming the surface.
Elevation: Higher altitudes generally experience lower temperatures due to decreased air pressure and thinner atmosphere, resulting in less heat retention.