Climate change in the UKOTs an overview of the ... - JNCC - Defra
Climate change in the UKOTs an overview of the ... - JNCC - Defra
Climate change in the UKOTs an overview of the ... - JNCC - Defra
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Sunlight<br />
passes<br />
through <strong>the</strong><br />
greenhouse<br />
gases <strong>an</strong>d<br />
warms <strong>the</strong><br />
earth<br />
Figure 6. Greenhouse effect<br />
Source: Impetus Consult<strong>in</strong>g Ltd.<br />
The greenhouse effect works much <strong>the</strong><br />
same way. Energy from <strong>the</strong> sun, or solar<br />
radiation, passes through <strong>the</strong> atmosphere<br />
<strong>an</strong>d warms <strong>the</strong> Earth’s surface. Some <strong>of</strong><br />
<strong>the</strong> radiation is reflected back out <strong>in</strong>to<br />
space at <strong>the</strong> level <strong>of</strong> <strong>the</strong> atmosphere.<br />
Some reaches <strong>the</strong> Earth, is absorbed by<br />
<strong>the</strong> ground <strong>an</strong>d released as heat. Some <strong>of</strong><br />
this heat passes back through <strong>the</strong> atmosphere<br />
<strong>in</strong>to outer space <strong>an</strong>d some is<br />
reta<strong>in</strong>ed by <strong>the</strong> gases <strong>in</strong> <strong>the</strong> atmosphere<br />
<strong>an</strong>d warms <strong>the</strong> Earth (Figure 6).<br />
This natural warm<strong>in</strong>g is what makes <strong>the</strong><br />
Earth habitable for <strong>the</strong> pl<strong>an</strong>ts, <strong>an</strong>imals <strong>an</strong>d<br />
hum<strong>an</strong>s that have evolved <strong>the</strong>re; without it,<br />
<strong>the</strong> Earth’s average temperature would be<br />
<strong>an</strong> <strong>in</strong>hospitable -18°C <strong>in</strong>stead <strong>of</strong> <strong>the</strong><br />
present 14°C.<br />
The enh<strong>an</strong>ced greenhouse effect<br />
When this natural warm<strong>in</strong>g process is<br />
exaggerated or enh<strong>an</strong>ced, <strong>the</strong>re is cause<br />
for concern. An <strong>in</strong>crease <strong>in</strong> <strong>the</strong> concentration<br />
<strong>of</strong> greenhouse gases <strong>in</strong> <strong>the</strong> atmosphere<br />
results <strong>in</strong> more heat be<strong>in</strong>g reta<strong>in</strong>ed<br />
<strong>an</strong>d <strong>an</strong> overall warm<strong>in</strong>g <strong>of</strong> <strong>the</strong> Earth’s temperature.<br />
Although <strong>the</strong>y make up a small<br />
percentage <strong>of</strong> atmospheric gases,<br />
<strong>ch<strong>an</strong>ge</strong>s <strong>in</strong> <strong>the</strong> concentration <strong>of</strong> greenhouse<br />
gases have a huge effect on <strong>the</strong> bal<strong>an</strong>ce<br />
<strong>of</strong> natural processes.<br />
34<br />
Greenhouse gases<br />
Atmosphere<br />
Outer Space<br />
The earth<br />
warms up <strong>an</strong>d<br />
gives out heat,<br />
some heat passes back out<br />
through <strong>the</strong> greenhouse gases<br />
but some is trapped <strong>in</strong>side<br />
keep<strong>in</strong>g <strong>the</strong> earth warm<br />
The hum<strong>an</strong> factor<br />
The core concern about climate <strong>ch<strong>an</strong>ge</strong> is<br />
hum<strong>an</strong> potential to alter <strong>the</strong> climate<br />
through activities that are a result <strong>of</strong> our<br />
way <strong>of</strong> life <strong>an</strong>d how we treat <strong>the</strong> natural<br />
environment. There have been signific<strong>an</strong>t<br />
Box 4. Hum<strong>an</strong> activity <strong>an</strong>d<br />
greenhouse gases<br />
The pr<strong>in</strong>cipal greenhouse gases<br />
that enter <strong>the</strong> atmosphere because<br />
<strong>of</strong> hum<strong>an</strong> activities are:<br />
Carbon Dioxide (CO 2 ): Carbon dioxide<br />
enters <strong>the</strong> atmosphere through <strong>the</strong> burn<strong>in</strong>g<br />
<strong>of</strong> fossil fuels (oil, natural gas, <strong>an</strong>d coal),<br />
solid waste, trees <strong>an</strong>d wood products, <strong>an</strong>d<br />
also as a result <strong>of</strong> o<strong>the</strong>r chemical reactions<br />
(e.g., m<strong>an</strong>ufacture <strong>of</strong> cement). Carbon dioxide<br />
is also removed from <strong>the</strong> atmosphere<br />
(or “sequestered”) when it is absorbed by<br />
pl<strong>an</strong>ts as part <strong>of</strong> <strong>the</strong> biological carbon cycle.<br />
Meth<strong>an</strong>e (CH 4 ): Meth<strong>an</strong>e is emitted dur<strong>in</strong>g<br />
<strong>the</strong> production <strong>an</strong>d tr<strong>an</strong>sport <strong>of</strong> coal,<br />
natural gas, <strong>an</strong>d oil. Meth<strong>an</strong>e emissions also<br />
result from livestock <strong>an</strong>d o<strong>the</strong>r agricultural<br />
practices <strong>an</strong>d by <strong>the</strong> decay <strong>of</strong> org<strong>an</strong>ic waste<br />
<strong>in</strong> municipal solid waste l<strong>an</strong>dfills.<br />
Nitrous Oxide (N 2 O): Nitrous oxide is<br />
emitted dur<strong>in</strong>g agricultural <strong>an</strong>d <strong>in</strong>dustrial<br />
activities, as well as dur<strong>in</strong>g combustion <strong>of</strong><br />
fossil fuels <strong>an</strong>d solid waste.<br />
Fluor<strong>in</strong>ated Gases: Hydr<strong>of</strong>luorocarbons,<br />
perfluorocarbons, <strong>an</strong>d sulfur hexafluoride<br />
are syn<strong>the</strong>tic, powerful greenhouse gases<br />
that are emitted from a variety <strong>of</strong> <strong>in</strong>dustrial<br />
processes. Fluor<strong>in</strong>ated gases are sometimes<br />
used as substitutes for ozone-deplet<strong>in</strong>g subst<strong>an</strong>ces<br />
(i.e., CFCs, HCFCs, <strong>an</strong>d halons).<br />
These gases are typically emitted <strong>in</strong> smaller<br />
qu<strong>an</strong>tities, but because <strong>the</strong>y are potent<br />
greenhouse gases, <strong>the</strong>y are sometimes<br />
referred to as High Global Warm<strong>in</strong>g Potential<br />
gases (“High GWP gases”).<br />
Source: US Environmental Protection Agency<br />
(www.epa.gov/climate<strong>ch<strong>an</strong>ge</strong>/emissions/<strong>in</strong>dex.html)