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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

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