Question

at latitudes both north and south of the equator light hits early surface at a non - perpendicular angle. as a result the diffused is more diffused (spread out). energy is transferred to each spot. the same amount of incoming is spread over larger and larger as you move away from the equator. which means the the temperature as the light has to travel farther. earth’s shape affects the angle that sunlight hits earth’s surface. the angle sunlight hits the surface affects the amount of energy transferred to parts of earth. because of the energy amounts of energy being transferred to different parts different locations are warmer or cooler throughout the year. different receive different amounts of throughout the year because the earth’s axis is tilted and not perpendicular to the sun. earth’s axis is tilted about 23.5 degrees so north pole appears to point at the same place in space throughout the year in the north - hemisphere. system. definition - is a set of connected parts that form a complex whole. during parts of the year the northern pole is tilted toward the sun. during this time the northern hemisphere is and experiencing summer. as the earth revolves around the sun, the northern hemisphere receives less and less direct sunlight which causes the temperature to cool. (autumn and winter). earth’s tilted axis results in the

Explanation:

The text discusses how the Earth's shape, the angle of sunlight hitting the Earth's surface, and the tilt of the Earth's axis affect the distribution of solar energy, leading to different temperatures in various parts of the Earth throughout the year. It also defines a system and relates it to the Earth - Sun system and the seasons.

Answer:

At latitudes both north and south of the equator light hits early surface at a non - perpendicular angle. As a result the sunlight is more diffused (spread out). Less energy is transferred to each spot. The same amount of incoming solar energy is spread over larger and larger areas as you move away from the equator. Which means the lower the temperature as the light has to travel farther. Earth’s shape affects the angle that sunlight hits Earth’s surface. The angle sunlight hits the surface affects the amount of energy transferred to different parts of Earth. Because of the varying amounts of energy being transferred to different parts different locations are warmer or cooler throughout the year. Different locations receive different amounts of solar energy throughout the year because the Earth’s axis is tilted and not perpendicular to the sun. Earth’s axis is tilted about 23.5 degrees, so North Pole appears to point at the same place in space throughout the year in the North - Hemisphere system. During parts of the year the Northern Pole is tilted toward the sun. During this time the northern hemisphere is warmer and experiencing summer. As the Earth revolves around the sun, the northern hemisphere receives less and less direct sunlight which causes the temperature to cool. (Autumn and Winter). Earth’s tilted axis results in the seasons because the tilt causes different amounts of sunlight to reach different parts of the Earth at different times of the year.