the tilt of the earths axis
The Earth's round shape and tilted axis cause variations in the amount of sunlight different places receive. The angle at which sunlight hits the Earth's surface changes as it revolves around the sun, leading to seasonal variations in daylight hours and intensity. This results in different regions receiving varying levels of direct sunlight throughout the year.
Because they receive more direct sunlight
The polar regions never receive any direct sunlight.
The latitude of an area on Earth affects the amount of sunlight it receives because it determines the angle at which sunlight hits the surface. Areas closer to the equator receive more direct sunlight as the sun is overhead, leading to warmer temperatures. In contrast, areas closer to the poles receive sunlight at a lower angle, spreading the energy over a larger area and resulting in colder temperatures.
equator
it is summer because in summer it is hot
The amount of direct solar energy at different areas of the Earth is affected by factors such as the angle of incoming sunlight, atmospheric conditions like cloud cover and pollution, and the Earth's axial tilt. Areas closer to the equator receive more direct sunlight throughout the year, while areas closer to the poles receive less direct sunlight due to the tilt of the Earth's axis.
The directness of sunlight affects the amount of energy received on Earth. When sunlight is more direct, less of it is scattered or absorbed by the atmosphere, leading to higher energy levels. This is why regions closer to the equator receive more direct sunlight and have higher energy potential compared to regions further from the equator where sunlight is less direct.
All continents receive direct sunlight for at least part of the year.
Because the rays of the sun is so hot it will heat any part of the earth witout being hit my direct sunlight
because it is 0 degrees
in august