Trends in global CO2 emissions - edgar - Europa
Trends in global CO2 emissions - edgar - Europa
Trends in global CO2 emissions - edgar - Europa
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production category (2A), we used the trend <strong>in</strong> lime<br />
production data for 2008–2011 (USGS, 2012) as proxy to<br />
estimate the trend <strong>in</strong> the other 2A <strong>emissions</strong>. All 2011 data<br />
are prelim<strong>in</strong>ary estimates.<br />
(4) Non-energy/feedstock uses of fuels<br />
(2B+2C+2D+2G+3+4D4):<br />
• ammonia production (2B1): net <strong>emissions</strong>, i.e.<br />
account<strong>in</strong>g for temporary storage <strong>in</strong> domestic urea<br />
production (for urea application see below);<br />
• other chemicals production, such as ethylene, carbon<br />
black, carbides (2B other);<br />
• blast furnace (2C1): net losses <strong>in</strong> blast furnaces <strong>in</strong> the<br />
steel <strong>in</strong>dustry, i.e. subtract<strong>in</strong>g the carbon stored <strong>in</strong> the<br />
blast furnace gas produced from the gross <strong>emissions</strong><br />
related to the carbon <strong>in</strong>puts (e.g., coke and coal) <strong>in</strong> the<br />
blast furnace as a reduc<strong>in</strong>g agent, s<strong>in</strong>ce the CO 2<br />
<strong>emissions</strong> from blast furnace gas combustion are<br />
accounted for <strong>in</strong> the fuel combustion sector (1A);<br />
• another source <strong>in</strong> metal production is anode<br />
consumption (e.g., <strong>in</strong> electric arc furnaces for secondary<br />
steel production, primary alum<strong>in</strong>ium and magnesium<br />
production) (2C);<br />
• consumption of lubricants and paraff<strong>in</strong> waxes (2G), and<br />
<strong>in</strong>direct CO 2<br />
<strong>emissions</strong> related to NMVOC <strong>emissions</strong><br />
from solvent use (3);<br />
• urea applied as fertiliser (4D4), <strong>in</strong> which the carbon<br />
stored is emitted as CO 2<br />
(<strong>in</strong>clud<strong>in</strong>g <strong>emissions</strong> from<br />
limestone/dolomite used for lim<strong>in</strong>g of soils).<br />
For the feedstock use for chemicals production (2B),<br />
ammonia production from USGS (2012) was used (2011<br />
data are prelim<strong>in</strong>ary estimates). S<strong>in</strong>ce CO 2<br />
<strong>emissions</strong> from<br />
blast furnaces are by far the largest subcategory with<strong>in</strong><br />
the metal production category 2C, for the trend <strong>in</strong> crude<br />
steel production for 2008–2009 USGS (2011) and for<br />
2009–2011 World Steel Association (WSA, 2012) was used<br />
to estimate the recent trend <strong>in</strong> the total <strong>emissions</strong>. For<br />
the very small <strong>emissions</strong> <strong>in</strong> categories 2G and 3, the<br />
2005–2008 trend was extrapolated to 2011. For simplicity,<br />
it was assumed that the small soil lim<strong>in</strong>g (4D4) <strong>emissions</strong><br />
follow the gross ammonia production trend.<br />
(5) Other sources (6C+7A):<br />
• waste <strong>in</strong>c<strong>in</strong>eration (fossil part) (6C)<br />
• fossil fuel fires (7A).<br />
The 2005–2008 trend was extrapolated to 2011 for the<br />
relatively very small <strong>emissions</strong> of waste <strong>in</strong>c<strong>in</strong>eration (6C)<br />
and underground coal fires (ma<strong>in</strong>ly <strong>in</strong> Ch<strong>in</strong>a and India)<br />
and oil and gas fires (1992, <strong>in</strong> Kuwait) (7A).<br />
CO 2<br />
<strong>emissions</strong> from underground coal fires <strong>in</strong> Ch<strong>in</strong>a and<br />
elsewhere have been <strong>in</strong>cluded <strong>in</strong> EDGAR 4.2, although the<br />
magnitude of these sources is very uncerta<strong>in</strong>. Van Dijk et<br />
al. (2009) concluded that CO 2<br />
<strong>emissions</strong> from coal fires <strong>in</strong><br />
Ch<strong>in</strong>a are at around 30 Tg CO 2<br />
per year. This is equivalent<br />
to about 0.3% of Ch<strong>in</strong>a’s CO 2<br />
<strong>emissions</strong> <strong>in</strong> 2011.<br />
A1.2 Other sources of CO 2<br />
<strong>emissions</strong>: forest and<br />
peat fires and post-burn decay<br />
The trend estimates of CO 2<br />
<strong>emissions</strong> do not <strong>in</strong>clude CO 2<br />
<strong>emissions</strong> from forest fires related to deforestation/<br />
logg<strong>in</strong>g and peat fires and subsequent post-burn<br />
<strong>emissions</strong> from decay of rema<strong>in</strong><strong>in</strong>g above ground<br />
biomass and from dra<strong>in</strong>ed peat soils. Although they are<br />
also significant but highly uncerta<strong>in</strong>, CO 2<br />
<strong>emissions</strong> from<br />
the decay of organic materials of plants and trees that<br />
rema<strong>in</strong> after forest burn<strong>in</strong>g and logg<strong>in</strong>g are also not<br />
<strong>in</strong>cluded. Annual CO 2<br />
<strong>emissions</strong> from peat fires <strong>in</strong><br />
Indonesia estimated by Van der Werf et al. (2008) <strong>in</strong>dicate<br />
that <strong>emissions</strong> from peat fires vary most around 0.1-0.2<br />
billion tonnes per year, except for peak years due to an El<br />
Niňo. For the very exceptional 1997 El Niňo, they<br />
estimated peat fire <strong>emissions</strong> at 2.5 billion tonnes CO 2<br />
.<br />
Joosten (2009) estimated <strong>global</strong> CO 2<br />
<strong>emissions</strong> from<br />
dra<strong>in</strong>ed peatlands <strong>in</strong> 2008 to amount 1.3 billion tonnes<br />
CO 2<br />
, of which 0.5 billion tonnes from Indonesia.<br />
A1.3 Data quality and uncerta<strong>in</strong>ties<br />
For <strong>in</strong>dustrialised countries, total CO 2<br />
<strong>emissions</strong> per<br />
country, accord<strong>in</strong>g to EDGAR 4.2, for the 1990–2008<br />
period, are generally with<strong>in</strong> 3% of officially reported<br />
<strong>emissions</strong>, except for a few economies <strong>in</strong> transition (EIT)<br />
(see examples provided <strong>in</strong> Table A1.1). Also most<br />
<strong>in</strong>dustrialised countries (Annex I) estimate the<br />
uncerta<strong>in</strong>ty <strong>in</strong> their reported CO 2<br />
<strong>emissions</strong> (exclud<strong>in</strong>g<br />
land use, IPCC sector 5) <strong>in</strong> the range of 2% to 5% (95%<br />
confidence <strong>in</strong>terval, equivalent to 2 standard deviations).<br />
The uncerta<strong>in</strong>ty <strong>in</strong> EDGAR’s total national CO 2<br />
<strong>emissions</strong><br />
from fossil fuel use and other, non-combustion sources is<br />
estimated at about 5% for OECD-1990 countries and<br />
around 10% for most EIT countries, such as Russia and the<br />
Ukra<strong>in</strong>e. For develop<strong>in</strong>g countries, the EDGAR uncerta<strong>in</strong>ty<br />
estimates of national CO 2<br />
<strong>emissions</strong> vary between 5% for<br />
countries with a well-developed statistical systems, such<br />
as India, and around 10% or more for countries with lessdeveloped<br />
statistical systems. This is based on the<br />
uncerta<strong>in</strong>ty <strong>in</strong> the fuel data discussed <strong>in</strong> the 2006 IPCC<br />
Guidel<strong>in</strong>es for greenhouse gas emission <strong>in</strong>ventories (IPCC,<br />
2006) and <strong>in</strong> the variation <strong>in</strong> the carbon content per fuel<br />
type, compared with IPCC default values (Olivier et al.,<br />
2010). Moreover, energy statistics for fast chang<strong>in</strong>g<br />
economies, such as Ch<strong>in</strong>a s<strong>in</strong>ce the late 1990s, and for the<br />
countries of the former Soviet Union <strong>in</strong> the early 1990s,<br />
are less accurate than those for the mature <strong>in</strong>dustrialised<br />
countries with<strong>in</strong> the OECD (Marland et al., 1999; Olivier<br />
Annexes | 25