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<strong>Falsification</strong> <strong>Of</strong> <strong>The</strong> <strong>Atmospheric</strong> CO 2 <strong>Greenhouse</strong> <strong>Effects</strong> . . . 31<br />

which may be integrated yielding<br />

T = T 0 +<br />

S<br />

ϱ c v d (t − t 0) (43)<br />

In this approximation, there is a linear rise of the temperature in time because of the irradiated<br />

intensity. One sees that the temperature rises particularly fast in absorbing bodies of small<br />

diameter: Thin layers are heated especially fast to high temperatures by solar radiation. <strong>The</strong><br />

same applies to the heat capacity per unit volume:<br />

• If the heat capacity is large the change of temperature will be slow.<br />

• If the heat capacity is small the change in temperature will be fast.<br />

Thus the irradiated intensity is responsible for the quick change of temperature, not for its<br />

value. This rise in temperature is stopped by the heat transfer of the body to its environment.<br />

Especially in engineering thermodynamics the different kinds of heat transfer and their<br />

interplay are discussed thoroughly [95–97]. A comprehensive source is the classical textbook<br />

by Schack [95]. <strong>The</strong> results have been tested e.g. in combustion chambers and thus have a<br />

strong experimental background.<br />

One has to distinguish between<br />

• Conduction<br />

• Convection<br />

• Radiation<br />

• Transfer of latent heat in phase transitions such as condensation and sublimation 9<br />

Conduction, condensation and radiation, which slow down the rise in temperature, work<br />

practically the same inside and outside the car. <strong>The</strong>refore, the only possible reason for a<br />

difference in final temperatures must be convection: A volume element of air above the ground,<br />

which has been heated by radiation, is heated up (by heat transfer through conduction), rises<br />

and is replaced by cooler air.<br />

This way, there is, in the average, a higher difference of<br />

temperatures between the ground and the air and a higher heat transmission compared to a<br />

situation, where the air would not be replaced. This happens inside the car as well, but there<br />

the air stays locked in and the air which replaces the rising air is getting warmer and warmer,<br />

which causes lower heat transmission. Outside the car, there is of course a lot more cooler air<br />

than inside. On the whole, there is a higher temperature for the sunlight absorbing surfaces<br />

as well as for the air.<br />

9 Among those phenomena governed by the exchange of latent heat there is radiation frost, an striking<br />

example for a cooling of the Earth’s surface through emission of infrared radiation.

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