Plants require sunlight to produce their food, without sunlight plants would die from starvation.
If the plants all died then the animals that eat plants (herbivores) would also run out of food and die of starvation.
If herbivores ran out of food and died then animals that eat other animals (carnivores) would run out of food and die of starvation.
Once all the plants and animals were gone, insects, bacteria and fungus would have no food supply left either and would also die.
This is an extreme example based on the loss of ALL sunlight. If the amount of sunlight were to just decrease then we would expect a much less extreme result. Less sunlight would result in less plant growth, less food for herbivores, less food for carnivores, etc. The amount of life that the earth could sustain would decrease but would not in my opinion disappear altogether.
When the sun is at a low angle, shadows are longer because the sunlight has to travel through more atmosphere before reaching the surface, thus making the shadows appear elongated. As the sun rises higher in the sky, shadows become shorter due to the more direct path of sunlight reaching the surface.
The sun is lower in the sky during winter due to the tilt of Earth's axis. This results in shorter days and less direct sunlight reaching the surface in the Northern Hemisphere where winter occurs from December to February.
The position of the Sun in the sky affects the intensity of sunlight striking Earth's surface primarily through the angle at which sunlight reaches the ground. When the Sun is higher in the sky, such as during midday, sunlight strikes the Earth more directly, leading to greater intensity and warmth. Conversely, when the Sun is lower on the horizon, sunlight arrives at a more oblique angle, spreading its energy over a larger area and reducing intensity. This variation is also influenced by seasonal changes and geographical location.
fire
Yes, the Earth's atmosphere is heated by solar energy. Sunlight penetrates the atmosphere and warms the surface of the Earth. This heat is then radiated back into the atmosphere, contributing to its overall temperature.
commonly 'sunlight', but more specifically UltraViolet radiation
The amount of sunlight reaching Earth's surface changes throughout the day due to the angle of the sun. Sunlight is strongest when the sun is directly overhead, typically around midday. As the sun moves lower in the sky in the morning and evening, the sunlight becomes more dispersed and less intense.
The amount of sunlight reaching a location at a particular time is determined by Earth's shape, axial tilt, rotation, and orbit around the sun. These factors affect the angle at which sunlight hits the Earth's surface, leading to variations in day length and intensity of sunlight throughout the year.
earths surface
Ozone
i belive so
When the sun is at a low angle, shadows are longer because the sunlight has to travel through more atmosphere before reaching the surface, thus making the shadows appear elongated. As the sun rises higher in the sky, shadows become shorter due to the more direct path of sunlight reaching the surface.
It blocks (some of) it from reaching the surface of the Earth.
It would block out significant sunlight, lowering the temperature.
The primary factor that affects the amount of solar energy reaching any point on Earth's surface is the angle at which the sunlight hits the surface. This angle, known as the solar zenith angle, determines the path length through the atmosphere that the solar radiation must travel, affecting the amount of absorption and scattering that occurs. The higher the angle, the more direct the sunlight, and the more energy that reaches the surface.
Different parts of Earth's surface receive different amounts of energy from the sun due to variations in the angle at which sunlight strikes the surface. This is influenced by factors such as the curvature of the Earth, the Earth's tilt on its axis, and the presence of clouds or other obstacles that can block or reflect sunlight.
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