What causes the sunlight to hit different latitudes on earth at different angles

The main factor that causes sunlight to hit different latitudes on Earth at different angles is the tilt of the Earth's axis. Earth's axis is tilted at an angle of approximately 23.5 degrees relative to its orbit around the Sun. This tilt causes the Sun's rays to hit different latitudes at different angles throughout the year.

During the summer solstice, the Northern Hemisphere is tilted towards the Sun, causing the Sun's rays to hit the Northern Hemisphere at a more direct angle. This results in longer days and warmer temperatures in the Northern Hemisphere. At the same time, the Southern Hemisphere is tilted away from the Sun, causing the Sun's rays to hit at a more oblique angle, resulting in shorter days and cooler temperatures.

Conversely, during the winter solstice, the situation is reversed, with the Southern Hemisphere experiencing longer days and warmer temperatures, while the Northern Hemisphere experiences shorter days and cooler temperatures.

The tilt of the Earth's axis also causes the changing seasons as the Earth orbits the Sun, with the angle of sunlight changing throughout the year. This tilt in combination with the Earth's orbit around the Sun causes the varying angles at which sunlight hits different latitudes on Earth.

The suns rate of burning fuel

The earths speed of rotation
The earths tilt on its axis or
The suns distance from earth

The Earth's tilt on its axis is the main factor that causes sunlight to hit different latitudes on Earth at different angles. The tilt of the Earth's axis is approximately 23.5 degrees relative to its orbit around the Sun, and this tilt is responsible for the changing seasons and the varying angles at which sunlight hits different latitudes.

The rate of burning fuel in the Sun, the Earth's speed of rotation, and the Sun's distance from Earth do not directly impact the angle of sunlight hitting different latitudes. However, the distance from the Sun does affect the intensity of sunlight and the Earth's temperature, while the Earth's speed of rotation determines the length of a day.