The ozone layer
ground radiation
Ultraviolet radiation is the solar radiation least absorbed by the layers of the atmosphere before reaching Earth. This is due to the ozone layer, which helps to absorb and block a significant portion of the incoming ultraviolet radiation.
Clouds and small particles of pollution, including volcanic emissions reflect some solar energy and prevent it reaching the ground.Ice and snow reflect the sun's energy too.The ozone layer also reflects some ultra-violet radiation.
The process that keeps solar energy from reaching the Earth and is measured by its albedo is reflection. Albedo refers to the fraction of solar energy reflected back into space by a surface, with higher albedo values indicating greater reflectivity. Surfaces such as clouds, ice, and snow have high albedo, reflecting a significant portion of incoming solar radiation, while darker surfaces absorb more energy. This reflection plays a crucial role in regulating the Earth's climate and temperature.
It blocks (some of) it from reaching the surface of the Earth.
It blocks Solar ultra-violet radiation from reaching Earth's surface.
A pyranometer is a device that measures the total solar radiation received from the sun. It is often used to quantify the heat radiation reaching the earth's surface.
Yes, polar latitudes receive less solar radiation than equatorial latitudes due to the Earth's axial tilt. This results in colder temperatures and less direct sunlight reaching the poles, creating a solar radiation deficit in these regions.
The function that provides insolation is solar radiation, specifically solar energy received by the Earth's surface. Insolation is the amount of solar radiation reaching a specific area over a given time period. It is an essential factor in understanding climate and ecosystems.
The term for the sun reflecting off the ground is called "solar reflection" or "ground reflection." This phenomenon can cause glare and increase the amount of sunlight reaching our eyes or solar panels.
No. Snow typically reflects much of the solar radiation reaching it, regardless of whether that is happening during an ice age or a warmer period.
The amount of solar energy reaching Earth is primarily controlled by three factors: the Earth's distance from the Sun, which varies due to its elliptical orbit; the Sun's output, which can fluctuate due to solar cycles; and the Earth's atmosphere, which can absorb or reflect solar radiation. Additionally, clouds and aerosols can influence how much solar energy reaches the surface. Together, these factors determine the overall solar radiation received by the planet.