The height of the sun in the sky changes due to the Earth's rotation. Because the Earth is rotating, the Sun appears to move, and unless you are on the equator, the sun will not move in a straight line. This is the apparent motion of the Sun and has been studied and modeled for 1000s of years.
There are numerous other factors that affect this as well including:
-Inclination of the Earth
-Earth's Revolution Around The Sun
-Earth's Orbit Not being a perfect circle
-Precession Of The Axes
-Instabilities in the Earth's Motion.
The sun does not change an angle. It is the earth that changes its tilt.
The earth has a natural tilt that affects how close any part of the globe is to the sun at any point in the year. For example, during June, July and August in the United States, it gets hot. That is because during those months the northern hemisphere is tilting toward the sun. But in Australia during June, July and August, it gets cold. That is because the Southern Hemisphere is tilting away from the sun during those months.
The angle of the rays of sunlight is important in determining the amount of energy collected by the earth. More direct sunlight means more energy received.
The earth's seasons are caused by the rotating earth tilting on its axis as it orbits round the sun. This tilting causes the sunlight to strike the earth at a low angle, causing winter in the hemisphere tilted away from the sun. Meanwhile, the hemisphere tilted towards the sun, receives the sunlight more directly, causing summer in the hemisphere tilted towards the sun.
The actual most important cause of Earth's seasons is it's axis.
season affect the way we live, the clothes we wear and the food we eat.
The Philippines must be closer to the equator giving them more sunlight. I'm sorry if my geography is off I didn't want to look at a map.
The angle of sunlight hitting the Earth affects the duration of daylight and intensity of sunlight received, influencing the changing seasons. In regions with more direct sunlight, there are longer days and higher temperatures, leading to summer. In contrast, areas with sunlight at a lower angle have shorter days and cooler temperatures, resulting in winter.
Beam spreading refers to the spreading out of solar radiation as it travels through Earth's atmosphere. During different seasons, the angle of incidence of sunlight changes due to the tilt of Earth's axis, which affects how much solar radiation is spread out over a larger area. This spreading out of sunlight is one of the factors that contribute to the changing seasons on Earth.
Earth's tilt causes the different seasons by changing the angle at which sunlight hits the Earth's surface. This variation in sunlight intensity creates differences in temperature and weather patterns across the globe. Regions closer to the poles experience more extreme seasons due to the tilt of the Earth's axis.
The angle of incidence refers to how directly sunlight strikes the Earth's surface. Seasonal changes occur because the Earth's tilt causes the angle of incidence to vary, affecting the amount of sunlight a given area receives. This variation in sunlight drives the changing seasons.
The Earth's tilt on its axis as it orbits the sun is what causes the seasons. This tilt affects the angle at which sunlight strikes the Earth's surface, leading to varying day length and intensity of sunlight throughout the year.
It affects seasons by the angle a planet is tilted.
Sunlight is at its strongest when it is at a perpendicular angle; at oblique angles it is weaker.
Seasons are primarily determined by the tilt of the Earth's axis and its orbit around the sun. The angle of sunlight, the length of daylight, and the amount of solar energy received by a particular hemisphere at any given time affect the temperature and weather patterns we experience during different seasons. Other factors, such as ocean currents and atmospheric circulation, can also influence regional climates.
Seasons depend on the tilt of the Earth's axis as it orbits the Sun. The angle of the Sun's rays hitting the Earth's surface changes throughout the year, causing different parts of the Earth to receive more or less sunlight, resulting in seasons.
The tilt of Earth's axis causes the seasons by affecting the angle at which sunlight hits the Earth's surface. When one hemisphere is tilted towards the sun, it receives more direct sunlight and experiences summer, while the opposite hemisphere is tilted away and experiences winter. As Earth orbits the sun, the tilt causes the seasons to change.
Seasons are caused by the tilt of Earth's axis as it orbits the Sun. The angle of the tilt affects the angle at which sunlight hits the Earth's surface, leading to variations in temperature and daylight hours throughout the year. This tilt results in different amounts of sunlight reaching different parts of the globe, creating the four seasons.
The seasons are primarily caused by the tilt of the Earth's axis, not its distance from the sun. This tilt results in different parts of the Earth receiving varying amounts of sunlight throughout the year, leading to the four seasons. The distance between the Earth and the sun does impact the intensity of sunlight received (which can affect climate in more subtle ways), but it's not the main driver of the seasonal changes.