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The Greenhouse Effect
Natural and Amplified Warming
The Sun
radiates thermal energy in all directions.
Before reaching the Earth, 1/3 of the solar radiations is
reflected back into space. Most of this
reflection is carried out by the clouds and the
aerosols. The rest is carried out by the
brighter features of the Earth: the snow, icebergs and deserts. On reaching the Earth, the balance
of 2/3
radiations is mostly absorbed by the Earth's surface.
Whatever is the amount of thermal radiations absorbed by the Earth, it has to be radiated back to the space, otherwise the Earth would be too warm for dwelling.
The Earth radiates thermal energy of lesser
energy (longer wavelengths) than the thermal energy it receives from
the Sun which is much hotter. For the Earth to reflect back thermal
radiations of these wavelengths, its surface would have to be mathematically be at a temperature of
- 19oC.
the actual temperature of the Earth is much warmer, 14o C, as we feel it now. This is due to the natural blanketing effect of the greenhouse gases which keeps the Earth about 33oC (14oC+19oC) warmer. Without these greenhouse gases in the atmosphere, the Earth would be too cold for living dwelling.
Man-Induced Greenhouse Effects
Unfortunately due to changes and new quality demands in our way of life, more energy is needed (for example increased cooling and heating systems in buildings, advanced infrastructure and transport system operating at bulleting speed, increased population with rapid economic growth in China, India and Brazil.) The related human activities have undesirably resulted in higher rate of greenhouse gas emission. The increased emission of the greenhouse gases, prominently, carbon dioxide, increases the blanketing effect. This means more radiations are trapped within the atmosphere, causing more warming. Snow and ice begin to melt. Since they also reflect the solar radiations, their disappearance means more solar radiations stay trapped in the Earth's atmosphere. The melting consequently exposes the darker lands and water surfaces beneath. Being darker, they absorb more radiations, causing more warming. This warming in turn causes more melting. This cascading effect is called the 'ice-albedo feedback'. It amplifies greenhouse effect and contributes to global warming. As a result of this greenhouse warming, higher rate of vaporization occurs at the oceans, producing more water vapor which is also a greenhouse gas. They reflect the solar radiations back to the Earth causing warming and generating more water vapor. The growing concern is the resultant excessive global warming; which has been shown to have altered, and will continue to alter global climate significantly.
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Reference and Related News:
Climate Change 2007 : The Physical Science
Basis - AR4 - IPCC
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