Insolation

Insolation is derived from the words "incoming solar radiation". Insolation is specifically applied to radiation which is arriving at earth’s atmosphere first and then earth's surface. The heat comes from solar energy. Insolation is the solar radiation that reaches the earth's surface. It is measured by the amount of solar energy received per square centimetre per minute. Solar energy received over the planet’s surface varies according to season, latitude, transparency of the atmosphere, and aspect, ground slope and albedo effect. 

Insolation affects temperature. The more the insolation, the higher the temperature.

In any given day, the strongest insolation is received at noon.

 Factors influencing insolation 
The amount of insolation received on the earth’s surface is not the same everywhere. It varies according to the place and time. Tropical regions get the most insolation, it gradually decreases towards the poles. Insolation happens more in summers and less in winters. The major factors which influence the amount of insolation received are:

 Solar constant
 The angle of incidence of the sun’s rays
 Duration of the day
Earth distance from Sun
 Transparency of the atmosphere

Solar Constant
At the top of the earth’s atmosphere, received insolation is expressed as the solar constant. It receives  at  the  top  of  the  atmospheric surface (thermopause) on  a perpendicular  plane  to the solar beam. The average insolation received at the thermopause i.e.1368Wm2 (Watt per squaremetre) energy(solar constant) is in the form of short wave. Thus, it is termed as solar constant for that  mean  distance  from  the  sun. These solar constant is varying  over 1 Wm2 by  periodic disturbances and explosions in the solar surface basically related to sun spot. Sun spots are dark and cooler areas visible on the sun’s surface. The recent researches have shown that more and more energy is released when the sunspots are in large number. The number of sunspots also increases or decreases on a regular basis, in a cycle of 11 years.

The angle of incidence

Since the earth is a geoid resembling a sphere, the sun’s rays strike the surface at different angles at different places. This depends on the latitude of the place. The higher the latitude, the less is the angle they make with the surface of the earth. The area covered by the vertical rays is always less than the slant rays. If more area is covered, the energy gets distributed and the net energy received per unit area decreases. Moreover, the sun’s rays with small angle traverse more of the atmosphere than rays striking at a large angle.

 How long is the day? 
The length of the day determines the duration of sunlight, which affects the amount of solar radiation received by the earth’s surface. The more hours of sunshine, the greater the quantity of solar radiation will be received by a particular place. For  example, at the  equator, days  and  nights are each 12 hours in all the months. In the  Arctic  and  Antarctic regions, the sunny time varies between 0 and 24 hours.  On the autumn and spring equinoxes (September and March respectively), the sun is overhead at the equatorial noon.  The night and day all over the earth are equal on these days. The maximum amount of insolation is received at the equator on those days, and the amount of insolation decreases towards  the  poles. This is because sunshine is  vertical at the equator but with increasing  latitudes, the rays become more  and  more  slanting. Therefore, poleward, the received energy flux is less.

Earth's Distance from Sun
The earth is revolving around the sun in an elliptical orbit, resulting continuous change in the distance between sun and the earth on annual basis. It leads to seasonal variation in solar energy received by the earth. The mean distance between the earth and sun is about 149,600,000 kilometers (92,900,000  miles). When earth position is farthest (152 million km) from sun is known as ‘aphelion’ on July  4. It is perihelion (147 million km) occurs on January 3 each year which is the closest distance. During aphelion the northern hemisphere is facing the sun and therefore receives energy about 7% less than the perihelion  (southern hemisphere).

Transparency of the Atmosphere 
Atmosphere is not transparent for all the radiation coming from the sun because of different composition and layers. It is also one of the controlling factors of insolation to reach earth surface. The  atmosphere is composed of gases, water vapour and particulate matters. The atmosphere is a mixture of gases: nitrogen (N), oxygen (O2), Argon, carbon dioxide, Neon (Ne), Helium (He), Methane (CH4), Krypton (Kr), Ozone (O3), Nitrous oxide (N2O), Hydrogen (H) and Xenon (Xe). The atmosphere also contains water vapour, water in the gaseous state.

The longer the duration of daylight, the more the insolation received per day.

 Other websites 
 National Science Digital Library - Insolation 
 Yesterday‘s Australian Solar Radiation Map

Category:Solar energy
Category:Climate