Wednesday, 28 March 2012


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The sun as the source of heat and light continually sends electromagnetic radiation into space. Part of this radiation is the visible light, the light that allows us to see during the day. Not all of the visible light transmitted by the sun reaches the surface of the earth. Some of the light energy is reflected back into space and some are absorbed by the atmosphere.

The atmosphere greatly changes the way sunlight reaches the surface of the earth. While sunlight travels through the atmosphere, air molecules and tiny suspended particles known as aerosols reflect, scatter and absorb the light energy. Thus the amount of sunlight present at the top of the earth’s atmosphere is lessened when it reaches the earth’s surface.

Aerosols responsible for scattering and absorbing sunlight are tiny liquid or solid particles that are suspended in atmosphere. Some aerosols occur naturally, originating from volcanoes, dust storms, forest and grassland fires, living vegetation, and sea spray. Human activities, such as the burning of fossil fuels and the alteration of natural surface cover, also generate aerosols.

Since aerosols change the way in which sunlight reaches the Earth’s surface, they also affect the way the climate of a certain geographical area changes. Scientists have much to learn about the way aerosols affect the regional and global climate. They have yet to accurately quantify the relative impacts on climate of natural aerosols and those of human origin. They are even unsure whether aerosols are warming or cooling our planet Earth. However, conducted scientific studies on aerosols suggest that aerosols really have a great impact on our global climate.

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