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