There are two general possibilities - depending upon several types of conditions -, it will be either reflected or absorbed.
Sunlight hits Earth's surface closer to the poles at a low angle, resulting in the energy being more spread out. This causes less intense sunlight and lower temperatures in polar regions compared to equatorial regions where sunlight hits more directly. The angle of sunlight hitting Earth's surface also contributes to the longer periods of darkness experienced in polar regions during their respective winter seasons.
The term for rain that freezes when it hits the earth's surface is freezing rain.
When sunlight hits Earth at an angle smaller than ninety degrees, the energy is spread over a larger surface area, resulting in less energy per unit area. This leads to lower intensity of sunlight and reduced heating compared to when sunlight hits directly overhead.
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.
As latitude increases, the intensity of solar radiation decreases. This is because the angle at which sunlight hits the Earth's surface becomes more oblique, leading to greater atmospheric absorption and scattering, which reduces the amount of solar energy that reaches the surface.
Sunlight that hits the Earth's surface is absorbed by the Earth. It is then reflected back.
i belive so
The sunlight will be absorbed by the surface.If the surface is a mirror,lesser light will be absorbed.More will be reflected. If the surface is black,more light will be absorbed.
a meteorite
Sunlight hits Earth's surface closer to the poles at a low angle, resulting in the energy being more spread out. This causes less intense sunlight and lower temperatures in polar regions compared to equatorial regions where sunlight hits more directly. The angle of sunlight hitting Earth's surface also contributes to the longer periods of darkness experienced in polar regions during their respective winter seasons.
It gets absorbed by the surface, reflected, and even radiated back as infrared rays where it is absorbed by the greenhouse gases in the atmosphere.
When sunlight hits a dark surface, the surface absorbs more of the light and converts it into heat compared to a light-colored surface. This absorption of light energy causes the dark surface to heat up more quickly, which is why dark surfaces can feel hotter to the touch than light-colored surfaces under direct sunlight.
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.
Direct rays of sunlight refer to sunlight that reaches the Earth's surface without being scattered or reflected by the atmosphere. This type of sunlight provides maximum intensity and warmth. It occurs when the sun is high in the sky and the angle of incidence is minimal.
Each beam of sunlight has the same amount of energy (which is where we get our warmth). The energy of the sun is more spread accross the Earth's surface with increased angles (oblique). This is what happens at the poles where the sun light hits the Earth at 180 degrees. It is cold at the poles because the sun's energy is spread out over a large area. As the angle of the sun decreases the energy of the sun hits the earth directly and is concentrate. This is what happens when the sun hits the equator at 90 degrees and that is why it is warm at the equator.
Each beam of sunlight has the same amount of energy (which is where we get our warmth). The energy of the sun is more spread accross the Earth's surface with increased angles (oblique). This is what happens at the poles where the sun light hits the Earth at 180 degrees. It is cold at the poles because the sun's energy is spread out over a large area. As the angle of the sun decreases the energy of the sun hits the earth directly and is concentrate. This is what happens when the sun hits the equator at 90 degrees and that is why it is warm at the equator.
The angle of incidence refers to the angle at which sunlight hits the Earth's surface. When sunlight hits the Earth's surface at a higher angle of incidence (more direct sunlight), the energy from the sunlight is more concentrated, leading to increased heating of the surface. This can result in higher temperatures on Earth.