The insolation only depends on the distance from the Sun.
On the Earth it's about 1.35 kW per square metre. For other planets you just divide by the square of the distance measured in astronomical units. It varies from about 15 kW per sq. m on Mercury to 1.5 W per sq. m on Neptune.
There is not a standard SI unit to measure sphericity.
Krumbein's sphericity is a measure of how closely a particle or grain approaches a sphere in shape. It is calculated as the ratio of the surface area of a sphere with the same volume as the particle to the surface area of the particle itself. The equation for Krumbein's sphericity is S = (pi^(1/3) * D^(1/3)) / A, where S is the sphericity, D is the volume equivalent diameter of the particle, and A is the surface area of the particle.
Venus is the hot planet with the runaway greenhouse effect. its oceans have boiled dry.
The angle of insolation affects the intensity of insolation directly. In other words, as the angle of insolation increases, so does the intensity of insolation because the Sun is directly overhead at Zenith, giving off direct, or vertical rays. The opposite happens when the angle of insolation decreases, causing a decrease in the intensity of insolation as well.
yes
Insolation, or incoming solar radiation, affects the Earth by providing energy for processes such as photosynthesis, evaporation, and the Earth's climate system. It plays a key role in driving weather patterns, ocean currents, and the overall climate of the planet. Changes in insolation can impact global temperatures and have implications for ecosystems and agriculture.
There is not a standard SI unit to measure sphericity.
insolation
Sunspots
Height and latitude affect levels of insolation, rain and humidity. See related questions.
Krumbein's sphericity is a measure of how closely a particle or grain approaches a sphere in shape. It is calculated as the ratio of the surface area of a sphere with the same volume as the particle to the surface area of the particle itself. The equation for Krumbein's sphericity is S = (pi^(1/3) * D^(1/3)) / A, where S is the sphericity, D is the volume equivalent diameter of the particle, and A is the surface area of the particle.
Yes, the angle of insolation would vary on a flat Earth due to the curvature of the planet. Areas closer to the Sun's direct rays would have a higher angle of insolation, resulting in more concentrated and intense sunlight, while areas farther away would have a lower angle of insolation, leading to less direct and less intense sunlight.
it can't be equal to 1
Insolation refers to the amount of solar radiation that reaches a given area. The duration of insolation varies throughout the day, with maximum exposure typically occurring around midday when the sun is highest in the sky. Factors such as time of year, latitude, and cloud cover can also affect the duration of insolation.
Direct and diffused insolation.
1
Insolation is a measurement of the solar radiation received by a surface over a unit time. It is an abbreviation for "incoming solar radiation."the amount of sunlight that reaches a planet.