So 50% reaches the surface of the earth (But 5% of that is reflected).
The solar radiation that reaches the earths surface from the sun is called INSOLATION
About 30% of incoming solar radiation is reflected back into space.Incoming solar radiation: 100%Reflected by the atmosphere: 6% : Absorbed by the atmosphere: 16%Continuing incoming solar radiation: 78%Reflected by clouds: 20% : Absorbed by clouds: 3%Continuing incoming solar radiation: 55%Reflected by the earth's surface: 4% : Absorbed by the earth's surface (lands and oceans): 51%(Source: NASA. see link below)A:Scientists use the term albedo to describe the percentage of solar radiation reflected back into space by an object or surface. A perfectly black surface has an albedo of 0 (all radiation is absorbed).A perfectly mirror-finished surface has an albedo of 1.0 (all radiation is reflected).Earth's average albedo is about 0.3. In other words, about 30 percent of incoming solar radiation is reflected back into space (from land, sea, clouds, ice and atmosphere) and 70 percent is absorbed.From point to point on the Earth's surface, the albedo varies; high for clouds or snow, low for cities and paved areas, intermediate for vegetation. Overall, averaging the bright areas with the cities, the Earth's albedo is about 0.3 or perhaps just a little higher; 0.34 or so.Well, all of it is not. Some of it is absorbed by the oceans, some by dry land, and some by the ice caps.
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The Earth's orbit affects rainfall patterns through variations in distance from the sun, which can influence the distribution and intensity of incoming solar radiation. These changes in solar radiation can impact atmospheric circulation patterns, which in turn, affect global weather systems and precipitation. Additionally, orbital parameters like eccentricity, tilt, and precession can influence long-term climate variations, such as ice ages.
Solar radiation from the sun is a major driver of Earth's climate. It warms the planet, controlling weather patterns and climate systems. Changes in solar radiation levels can influence temperature variations and impact the Earth's climate in both short and long-term scales.
Radiation is the general term describing the type of energy transfer - insolation means incoming solar radiation, referring specifically to that which comes from the sun to the earth.
The solar radiation that reaches the earths surface from the sun is called INSOLATION
Radiation refers to the emission of energy in the form of electromagnetic waves or particles. Insolation specifically refers to the amount of solar radiation received by a specific area, typically measured over a given period of time. In essence, insolation is a subset of radiation, focusing solely on solar energy reaching the Earth's surface.
Radiation is a general term for the energy transmitted through space.Incident radiation is a term used when referring to the radiation hitting a specific surface. For instance, the incident radiation for a solar panel is the total amount of radiation hitting the surface of the solar panel. This is in contrast to direct beam radiation which refers to only that radiation which arrives in a strait line from the sun. (It differs in that total incident radiation includes additionally the component of diffuse radiation.)
Radiation energy is a broad term that includes various forms of energy, such as electromagnetic radiation and particle radiation. Solar energy specifically refers to the radiant energy emitted by the Sun, which is a type of electromagnetic radiation. Therefore, solar energy is a subset of radiation energy.
About 30% of incoming solar radiation is reflected back into space.Incoming solar radiation: 100%Reflected by the atmosphere: 6% : Absorbed by the atmosphere: 16%Continuing incoming solar radiation: 78%Reflected by clouds: 20% : Absorbed by clouds: 3%Continuing incoming solar radiation: 55%Reflected by the earth's surface: 4% : Absorbed by the earth's surface (lands and oceans): 51%(Source: NASA. see link below)A:Scientists use the term albedo to describe the percentage of solar radiation reflected back into space by an object or surface. A perfectly black surface has an albedo of 0 (all radiation is absorbed).A perfectly mirror-finished surface has an albedo of 1.0 (all radiation is reflected).Earth's average albedo is about 0.3. In other words, about 30 percent of incoming solar radiation is reflected back into space (from land, sea, clouds, ice and atmosphere) and 70 percent is absorbed.From point to point on the Earth's surface, the albedo varies; high for clouds or snow, low for cities and paved areas, intermediate for vegetation. Overall, averaging the bright areas with the cities, the Earth's albedo is about 0.3 or perhaps just a little higher; 0.34 or so.Well, all of it is not. Some of it is absorbed by the oceans, some by dry land, and some by the ice caps.
The term used to describe the Sun and the planets that orbit around it is "solar system."
Solar is a term used to define anything that relates to the sun. Solar panels and heat, relies on energy from the sun.
Insolation, or solar radiation.
Nativism
Big Bang is the term that describes how the solar system was formed.
Radioactive elements.