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Manual for Refrigeration Servicing Technicians - UNEP - Division of ...

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1<br />

Environmental Impact<br />

Global warming<br />

The earth’s temperature is maintained by a balance between<br />

heating from solar radiation flowing in from the sun, and cooling<br />

from infrared radiation emitted by the earth’s warm surface and<br />

atmosphere escaping back to into space. The sun is the earth’s only<br />

external source <strong>of</strong> heat. When solar radiation, in the <strong>for</strong>m <strong>of</strong> visible<br />

light, reaches the earth, some is absorbed by the atmosphere and<br />

reflected from clouds and land (especially from deserts and snow).<br />

CHAPITRE 1<br />

The remainder is absorbed PAGE 24 by the surface which is heated and in<br />

THE CONCEPT OF GLOBAL WARMING<br />

turn warms the atmosphere. The warm surface and atmosphere<br />

<strong>of</strong> the earth emit invisible infrared radiation. While the atmosphere<br />

is relatively transparent to solar radiation, infrared radiation is<br />

absorbed in the atmosphere by many less abundant gases. Though<br />

present in small amounts, these trace gases act like a blanket,<br />

preventing much <strong>of</strong> the infrared radiation from escaping directly<br />

to space. By slowing<br />

SUN<br />

the release <strong>of</strong> cooling<br />

SUN’S RADIATION<br />

radiation, these gases<br />

warm the earth’s surface.<br />

This process is illustrated<br />

here:<br />

GREENHOUSE GASES<br />

EARTH<br />

TROPOSPHER<br />

INFRARED RADIATION BEING TRAPPED<br />

The concept <strong>of</strong> global warming<br />

In a greenhouse, glass allows sunlight in but prevents some infrared<br />

radiation from escaping. The gases in the earth’s atmosphere<br />

which exert a similar effect are called “greenhouse gases” (GHGs).<br />

Of the man-made greenhouse gases, the most important are<br />

carbon dioxide (CO2), methane (CH4), nitrous oxide (N2O), and the<br />

halocarbons (CFCs, HCFCs and HFCs).<br />

Different gases absorb and trap varying amounts <strong>of</strong> infrared<br />

radiation. They also persist in the atmosphere <strong>for</strong> differing time<br />

periods and influence atmospheric chemistry (especially ozone) in<br />

different ways. For example, a molecule <strong>of</strong> R12 has about the same<br />

effect on radiation as 16,000 CO2 molecules. A molecule <strong>of</strong> methane<br />

has approximately 21 times the effect <strong>of</strong> CO2; but its lifetime is far<br />

shorter. The GWP is an index which compares the warming effect<br />

over time <strong>of</strong> different gases relative to equal emissions <strong>of</strong> CO2<br />

(by weight). A table <strong>of</strong> the ODP and GWP <strong>of</strong> various refrigerants<br />

is included in Chapter 2. HFCs do not have chlorine, and in this<br />

way, don’t destroy the ozone layer, but they do contribute to global<br />

warming. For this reason, they are in the group <strong>of</strong> gases controlled<br />

by Kyoto Protocol. These gases are: CO2, CH4, N2O, HFCs,<br />

perfluorocarbons (PFCs) and sulphur hexafluoride (SF6).<br />

Scientific measurements have shown that in the last century, the<br />

Earth’s average near-surface atmospheric temperature rose 0.6 ± 0.2<br />

°C, mostly attributable to human activities increasing the concentration<br />

<strong>of</strong> CO2 and other greenhouse gases in the atmosphere. Moreover, a<br />

global temperatures increase by between 1.4 and 5.8 °C between 1990<br />

and 2100 has been predicted by the models and disseminated by the<br />

Intergovernmental Panel on Climate Change (IPCC).<br />

24

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