Want this question answered?
Intensity of insolation refers to the intensity of the sun's rays on the earth's surface. It is a measure of solar energy that is received by a given surface area at a given time.
Normal to the Sun's rays, very roughly 1kW per m^2
The angle of insolation into a surface is largest when the surface directly faces the Sun. That coincides with the temperature rising. So the angle of insolation goes up as the temperature goes up.
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.
Insolation is the amount of the Sun's energy reaching a unit surface area on Earth (for example energy per square metre). Insolation is reduced with increasing latitude, because of the angle at which the Sun's rays hit the surface. The changing angle at which the energy hits the surface means that the energy is spread over a larger area with increasing latitude, North or South. That's the main reason the poles are cold and the equator is hot. In the hemisphere where it's summer, the effect is not so extreme because of the Earth's axial tilt ("towards" the Sun, in that hemisphere). In the winter time at high latitudes the effect is very significant because the Earth is then "tilted away" from the Sun, in that hemisphere.
As the altitude of the sun increases, the intensity of insolation for that area will increase as well.
Intensity of insolation refers to the intensity of the sun's rays on the earth's surface. It is a measure of solar energy that is received by a given surface area at a given time.
Normal to the Sun's rays, very roughly 1kW per m^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.
clouds, angle of instance, materials that absorb the suns energy, pollution, and objects
Latitude and altitude can dramatically affect climate and vegetation. Climate and altitude both have an effect on temperature. This temperature is a big factor in what will grow and what will not.
the approximate intensity of the sun is about 15millionK
Insolation
you can measure the angle of insolation by measuring the angle of the shadows that appear
The albedo effect is how a darker material gets hotter faster than a lighter material. Insolation is the solar radiation from the sun.
Insolation, or solar radiation.
The angle of insolation into a surface is largest when the surface directly faces the Sun. That coincides with the temperature rising. So the angle of insolation goes up as the temperature goes up.