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Post 2015: Global Action for an Inclusive and Sustainable Future

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6.3.1 Atmosphere <strong>an</strong>d global warming<br />

there is a broad academic <strong>an</strong>d policy consensus<br />

that increased greenhouse gas (GHG) emissions<br />

<strong>an</strong>d atmospheric concentrations have led to rising<br />

global temperatures. In fact, 2000–2009 was the<br />

warmest decade since records beg<strong>an</strong> in the mid-<br />

19th century. current models project that GHG<br />

emissions could double over the next 50 years,<br />

which would lead to at least a 3°c rise in the global<br />

temperature by the end of the century (unEp,<br />

2012b). the oEcD (2012) projects a smaller<br />

increase in GHG emissions by 2050 (50%), but<br />

also projects that the global temperature could rise<br />

between 3°c <strong>an</strong>d 6°c by 2100. a key contributing<br />

factor is the level of energy-related carbon-dioxide<br />

(co2) emissions, which is expected to grow by 70%<br />

by 2050 (oEcD, 2012). these trends could have<br />

subst<strong>an</strong>tial economic impacts.<br />

Some estimates suggest that a 2.5°c temperature<br />

increase from pre-industrial levels could generate<br />

economic damages equivalent to 1–2% of world<br />

GDp by 2100. these values rise signific<strong>an</strong>tly under<br />

alternative scenarios: 2–4% of world GDp with a<br />

4°c temperature increase, <strong>an</strong>d 10–11% of global<br />

GDp with a 6–7°c increase (unEp, 2012a). the<br />

environmental, social <strong>an</strong>d economic consequences<br />

of such scenarios would be catastrophic.<br />

the main effects of a signific<strong>an</strong>t long-term rise<br />

in global temperature include ch<strong>an</strong>ges to rainfall<br />

patterns, rising sea levels <strong>an</strong>d greater intensity <strong>an</strong>d<br />

frequency of extreme weather events. Flood <strong>an</strong>d<br />

drought-related disasters have risen by 230% <strong>an</strong>d<br />

38% respectively between the 1980s <strong>an</strong>d 2000s,<br />

while the costs of adaptation <strong>an</strong>d mitigation of<br />

these events are also expected to soar (unEp,<br />

2012a). the poorest regions are expected to be<br />

the worst affected by the consequences of climate<br />

ch<strong>an</strong>ge (cline, 2007). africa <strong>an</strong>d asia, in particular,<br />

will experience reduced agricultural productivity<br />

<strong>an</strong>d food security, increased water stress, floods<br />

<strong>an</strong>d droughts, <strong>an</strong>d the spread of diseases such as<br />

cholera (Ipcc, 2007). Small isl<strong>an</strong>d development<br />

states (SIDS), especially in the caribbe<strong>an</strong> <strong>an</strong>d<br />

pacific regions, are also extremely vulnerable to<br />

environmental shocks. climate ch<strong>an</strong>ge will also<br />

cause signific<strong>an</strong>t biodiversity losses.<br />

Increased air pollution could generate large<br />

economic losses, <strong>for</strong> inst<strong>an</strong>ce by lowering agricultural<br />

yields <strong>an</strong>d accentuating the impacts described<br />

above. moreover, it would aggravate its already large<br />

impact on global health, in particular respiratory<br />

diseases. air pollution is expected to become the<br />

main environmental cause of premature deaths<br />

by 2050, overtaking unsafe water <strong>an</strong>d s<strong>an</strong>itation<br />

(oEcD, 2012). this is partly due to increased traffic<br />

<strong>an</strong>d industrial emissions, which raise pollution<br />

concentrations in urb<strong>an</strong> areas, but also due to high<br />

domestic pollution from biomass cooking stoves.<br />

there has been some progress in protecting the<br />

stratospheric ozone. For example, the measures taken<br />

under the 1987 montreal protocol were instrumental<br />

in drastically reducing the consumption of ozonedepleting<br />

subst<strong>an</strong>ces, which in turn have led to a<br />

signific<strong>an</strong>t decline in their concentration in the<br />

stratosphere since 1994 (unEp, 2012a). this is <strong>an</strong><br />

encouraging illustration of how a global agreement<br />

c<strong>an</strong> lead to successful results.<br />

6.3.2 L<strong>an</strong>d<br />

about one-third of the world’s l<strong>an</strong>d surface is<br />

currently used <strong>for</strong> agricultural production, with<br />

<strong>an</strong>other third occupied by <strong>for</strong>ests, <strong>an</strong>d a fifth by<br />

sav<strong>an</strong>nahs <strong>an</strong>d grassl<strong>an</strong>ds. the remaining l<strong>an</strong>d is<br />

sterile or unproductive, with cities covering only<br />

1% of the global l<strong>an</strong>d mass (Hertel, 2010).<br />

the increasing pressures on l<strong>an</strong>d are due partly to<br />

competing dem<strong>an</strong>ds <strong>for</strong> food, <strong>an</strong>imal feed, fuel, fibre<br />

<strong>an</strong>d raw materials, which aggravate de<strong>for</strong>estation<br />

<strong>an</strong>d desertification (unEp, 2012b). the factors<br />

underlying these trends include population growth,<br />

ch<strong>an</strong>ging consumption patterns associated with<br />

improved living st<strong>an</strong>dards <strong>an</strong>d the search <strong>for</strong><br />

alternative sources of energy.<br />

poSt-<strong>2015</strong>: <strong>Global</strong> actIon For <strong>an</strong> IncluSIvE <strong>an</strong>D SuStaInablE FuturE<br />

Some estimates<br />

suggest that a<br />

2.5°C temperature<br />

increase from preindustrial<br />

levels<br />

could generate<br />

economic<br />

damages<br />

equivalent to<br />

1–2% of world<br />

GDP by 2100.<br />

These values rise<br />

signific<strong>an</strong>tly<br />

under alternative<br />

scenarios: 2–4% of<br />

world GDP with a<br />

4°C temperature<br />

increase, <strong>an</strong>d<br />

10–11% of global<br />

GDP with a 6–7°C<br />

increase.<br />

95

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