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 determines the roundness of a rock. The forumal is the cube root of DsDi/Di^2
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.
The law of universal gravitation
Yes
insolation
There is not a standard SI unit to measure sphericity.
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Krumbein's sphericity determines the roundness of a rock. The forumal is the cube root of DsDi/Di^2
When Earth revolves around the sun different areas will get different amounts of insolation. For example, in the Northern Hemisphere our winter days are shorter and summers are longer.
Height and latitude affect levels of insolation, rain and humidity. See related questions.
it can't be equal to 1
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.
Insolation is a measurement of the solar radiation received by a surface over a unit time. Polar regions have the lowest insolation.
The distance between the sun and a planet determines its orbital period, its orbital speed, and the amount of insolation. Other factors such as composition and albedo are required to determine other variables.