Emissions Scenarios - IPCC
Emissions Scenarios - IPCC
Emissions Scenarios - IPCC
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Emission <strong>Scenarios</strong> 269<br />
technically possible to reduce the anode emissions by a factor<br />
of 10 (EU, 1997). This technically feasible reduction can be<br />
achieved by changing from the Soderberg cells currently in use<br />
to more modern pre-bake cells. It is assumed that this will<br />
happen in the Al and Bl family scenarios, in which specific<br />
emissions of 0.15 kgCF^/t are achieved by 2040 in the<br />
OECD90 region and by 2090 in the other regions. In the A2<br />
and B2 family scenarios the same specific emissions are<br />
achieved later in the century in the OECD90 region and not<br />
until after 2100 in the other regions.<br />
PFCs are consumed in small amounts in such sectors as<br />
electronics (tracers), cosmetics, and medical applications.<br />
However, the only emissions included in Fenhann (2000)<br />
beyond aluminum production were PFCs (as CF^) from<br />
semiconductor production. In all SRES scenarios the emission<br />
estimates used are those given by Hamisch et al. (1999) of 0.3<br />
kt CF4 per year in 1990, 1.1 ktCF^ in 2000, 1.0 ktCF^ in 2010,<br />
and constant thereafter. The use of these estimates reflects the<br />
voluntary agreement, in April 1999, of the World<br />
Semiconductor Council, which represent manufacturers from<br />
Europe, Japan, Korea, and the US, among others. According to<br />
this agreement, manufacturers have adopted the emission<br />
reduction target for PFCs of 10% absolute reduction from 1995<br />
emission levels by 2010. This target encompasses over 90% of<br />
the total semiconductor production (WMO/UNEP, 1999). The<br />
total PEC emissions in the four SRES scenario families cover<br />
a range from 24 to 97 kt PFC in 2100 (Table 5-8; Fenhann,<br />
2000).<br />
5.4.3.3. Sulfur hexafluoride<br />
SFg is an extremely stable atmospheric trace gas. All studies<br />
concur that this gas is entirely anthropogenic. Its unique<br />
physico-chemical properties make SFg ideally suited for many<br />
specialized industrial applications. Its 100-year GWP of<br />
23,900 is the highest of any atmospheric trace gas. In 1994,<br />
atmospheric concentrations of SFg were reported to rise by<br />
6.9% per year, which is equivalent to annual emissions of<br />
5,800 tSFg (Maiss et al, 1996).<br />
According to several sources (Kroeze, 1995; Maiss et al,<br />
1996; Victor and MacDonald, 1998), about 80% of SFg<br />
emissions originate from its use as an insulator in high-voltage<br />
electrical equipment. The remaining 20% of the present global<br />
SFg emissions (1200 tons per year) are emitted from<br />
magnesium foundries, in which SFg is used to prevent<br />
oxidation of molten magnesium. The global annual production<br />
of magnesium is about 350,000 tons (US Geological Survey,<br />
1998), and developing countries account for about 15% of the<br />
total. SFg is also used to de-gas aluminum, but since SFg reacts<br />
with aluminum, little or no atmospheric emissions result from<br />
this process.<br />
Major manufacturers of SFg agreed voluntarily to co-operate<br />
on the compilation of worldwide SFg sales data by end-use<br />
markets. Six companies from the US (three), Japan, Italy, and<br />
Germany participated in the data survey. The companies do not<br />
expect the total sales for magnesium foundries to increase<br />
before 2000 (Science & Policy Services Inc., 1997). Based on<br />
this information, the 1996 statistical production values were<br />
used for the year 2000 in the fomiulation of the scenarios<br />
reported in Fenhann (2000). Future production was projected<br />
assuming the same consumption elasticity to GDP as for<br />
aluminum (see discussion above). In 1996, about 41% of the<br />
world magnesium was produced in the US; of this, only 16%<br />
was processed in foundries for casting that resulted in<br />
emissions of SFg (Victor and MacDonald, 1998). Since the<br />
distribution of world foundry capacity appears to be roughly<br />
similar to that of world magnesium production, Fenhann<br />
(2000) assumes that, presently, 16% of the produced<br />
magnesium is processed in foundries across all regions.<br />
Relating this amount of the processed magnesium to the<br />
aforementioned emission of 1200 tSFg per year yields an<br />
emission factor of 21 kgSFg per ton of magnesium processed in<br />
foundries. The demand for magnesium in automotive<br />
applications as a strong lightweight replacement for steel is<br />
growing quickly. Hence, it is expected that the fraction of total<br />
magnesium production processed in foundries by 2050 will<br />
grow to between two to three times the present level.<br />
As mentioned above, no less than 80% of SFg emissions (or<br />
4600 tons of SFg per year at present) originate from the use of<br />
SFg as a gaseous insulator in high-voltage electrical equipment.<br />
The unique ability of SFg to quench electric arcs has enabled<br />
the development of safe, reliable gas-insulated high-voltage<br />
breakers, substations, transformers, and transmission lines. The<br />
demand for such electrical equipment is assumed to grow<br />
proportionally to electricity demand (Victor and MacDonald,<br />
1998; Fenhann, 2000) with an emission factor of 132.6 tSFg/EJ<br />
electricity. Fenhann (2000) used preliminary electricity<br />
generation projections from the four SRES marker scenarios<br />
and assumed additional various other potentials for emission<br />
reductions that result from more careful handling, recovery,<br />
recycling, and substitution of SFg. Reduction rates vary in the<br />
different SRES scenario storylines; the detailed assumptions<br />
are reported in Fenhann (2000). The SFg emissions for the four<br />
scenarios given in Fenhann (2000) range from 7 to 25 ktSFg in<br />
2100. The main driver is electricity consumption, since the<br />
bulk of emissions originate from electric power transmission<br />
(for transformers).<br />
SFg is also emitted from other minor sources, but for the<br />
purposes of this report it is assumed that uncertainty ranges<br />
factored into the alternative scenario formulations cover the<br />
emissions from these sources.<br />
5.5. Aerosols and Ozone Precursors<br />
In addition to the GHGs discussed above, aerosol particles and<br />
tropospheric ozone also change the radiative balance of the<br />
atmosphere, albeit in a spatially heterogeneous manner. Sulfate<br />
aerosol particles, which form as a consequence of SOj<br />
emissions, act as a cooling agent. Their net effect is quite<br />
uncertain, but is thought to offset the forcing from all ПОП-СО2