What causes days to be warmer on one part of Earth than on another? (1 point) Responses the angle at which the sun strikes Earth the angle at which the sun strikes Earth the number of cars on the road the number of cars on the road the rotation of Earth the rotation of Earth the speed of Earth in its orbit
The angle at which the sun strikes Earth.
The angle at which the sun strikes Earth is the main factor that causes days to be warmer on one part of Earth than on another. The rotation of Earth and the speed of Earth in its orbit also play a role in the overall distribution of warmth and coolness on different parts of the planet. However, the angle at which the sun's rays hit the Earth's surface determines the intensity of solar radiation received in a particular area, leading to variations in temperature. The number of cars on the road does not directly affect the temperature distribution on Earth.
The angle at which the sun strikes Earth and the rotation of Earth are the factors that cause days to be warmer on one part of the Earth than on another. However, the speed of Earth in its orbit and the number of cars on the road are not direct causes of temperature differences between different parts of the Earth.
To understand why days can be warmer in one part of the Earth compared to another, we need to consider the angle at which the sun's rays hit the Earth's surface. The Earth is a sphere, so the angle at which sunlight reaches different parts of the Earth varies throughout the day and across different latitudes.
When the sun is high in the sky, the sunlight reaches a smaller area of the Earth's surface, and the rays are more concentrated. This results in more heating and warmer temperatures. Conversely, when the sun is at a lower angle in the sky, the sunlight is spread over a larger area, making it less concentrated and resulting in cooler temperatures.
Additionally, the rotation of the Earth plays a role in temperature variations. As the Earth rotates on its axis, different parts of the planet are exposed to the sun's rays for different lengths of time. This creates variations in the duration of daylight, which affects the amount of solar energy received and therefore the temperature.
In summary, the angle at which the sun strikes Earth and the rotation of Earth are the primary factors that cause variations in temperature between different parts of the Earth.