National Atmospheric Emissions Inventory

Introduction

Increasing atmospheric concentrations of greenhouse gases originating from man’s activities are leading to enhanced warming of the atmosphere and global climate change. The major greenhouse gases are carbon dioxide (CO2), methane (CH4) and nitrous oxide (N2O) all of which have both natural and anthropogenic sources. In contrast, the three industrial gases: hydrofluorocarbons (HFC), perfluorocarbons (PFC) and sulphur hexafluoride (SF6), are potent greenhouse gases but do not occur in nature, and hence only originate from anthropogenic sources.

These six greenhouse gases comprise the ‘basket of emissions’ against which reduction targets were agreed at the Third Conference of the Parties of the United Nations Framework Convention on Climate Change in Kyoto, Japan in December 1997. The target for the UK is to achieve a reduction of the global warming potential of the six greenhouse gases of 12.5% by 2008-2012 (based on 1990 emissions estimates). Consequently the UK are required to compile annual emission inventories of these greenhouse gases, and report the emissions to international bodies, to demonstrate compliance with this legislation. This is done within a reporting framework to ensure accuracy and consistency, although data is presented here in a UN/ECE reporting format (see Appendix 4). More detailed information may be found in the annual report on UK GHG emissions produced by the NAEI (Salway 1999).

The 1998 emissions for each of these six greenhouse gases are summarised in Table 2.1, and their inventories are discussed in the following sections. Inventories for the three indirect greenhouse gases (carbon monoxide, nitrogen oxides and non-methane volatile organic compounds) are included in subsequent chapters (Chapters 4, 5 and 5 respectively).

The total global warming potential of UK greenhouse gas emissions has been calculated using their global warming potentials (GWPs), which measures their effectiveness in global warming relative to CO2, agreed by IPCC for a 100 year time horizon (IPCC, 1996).

Table 2.1 GWP for UK Emissions of Greenhouse Gases in 1998

Direct GHG

Emissions (kt)
in 1998

GWP

(100 years)

Global Warming Equivalence - emissions GWP
(equivalent kt of CO
2)

CO2

572,9021

1

572,902

CH4

2,637

21

55,354

N2O

181

310

55,983

HFCs

3.656

560-121002

20,183

PFCs

0.094

6000-74002

652

SF6

0.054

23900

1,289

1 Calculated on IPCC basis and includes land-use change emissions. CO2 includes emissions only and does not include land use change and forestry removals

2 Range of GWP for species used

During the period 1990-1998 there has been a decrease in UK emissions of CO2, CH4, N2O and PFC but considerable increases in HFC and SF6 emissions. The overall effect has been a decrease in global warming potential from UK emissions. Figure 2.1 shows greenhouse gas emissions (comprising CO2 , CH4 , N2O , HFCs, PFCs and SF6) as CO2 equivalent for 1990 to 1998. Reliable emission estimates of HFCs, PFCs, SF6 and N2O (from adipic acid production) are not available prior to 1990.

Figure 2.1 Total Global Warming Potential Associated with UK Emissions of GHGs

Carbon dioxide is the major contributor to the UK’s greenhouse gas emissions and arises predominately from the combustion of fossil fuels. Non-fossil fuel sources are more difficult to assess due to the importance of CO2 in respiratory processes and its role within the global carbon cycle. Following internationally agreed conventions, the NAEI excludes emissions of CO2 originating from recently photosynthesised carbon as these will be part of the "carbon cycle". Hence emissions from biomass combustion, the organic component of waste incineration, landfill and sewage treatment are not included in the total. Emissions of other pollutants from biomass combustion are included in the appropriate inventories. The NAEI also currently excludes CO2 emissions from the effect of changing land use although these emissions are estimated in the UK Greenhouse Gas Inventory (Salway, 1999) and are discussed below.

Methane, like carbon dioxide, is naturally occurring and is part of the global carbon cycle. However, the magnitudes of sinks and sources of methane are not well known. Methane in the atmosphere is eventually oxidised to CO2 and the most recent IPCC estimate of its lifetime in the atmosphere is 12±3 years (IPCC, 1996). Methane has a much greater warming effect on the climate than carbon dioxide (Table 2.1). The major anthropogenic sources of methane are waste disposal, agriculture, coal mining and leakage from the gas distribution system. Due to the nature of these sources the estimation of methane emissions is very uncertain although the methodologies are continuously being improved. Early estimates of methane emissions by sector were based on the findings of the Watt Committee on Energy (Williams, 1994), however many have now been revised to take into account new information and to ensure consistency with the methodologies recommended by the IPCC 1996 Revised Guidelines (IPCC, 1997).

The third direct greenhouse gas, nitrous oxide (N2O), is emitted from natural and anthropogenic sources (agriculture, biomass burning, coal combustion and some industrial processes). As N2O has a GWP of 310, it is a powerful greenhouse gas. However, emissions from the UK are low, so the overall contribution to global warming is relatively small (although still significant). A full set of detailed emission factors for man-made sources, e.g. combustion, are not yet available however emissions are estimated using the default values given in the guidelines and more detailed data on coal combustion based on UK literature.

The three industrial greenhouse gases included in the ‘basket of emissions’ agreed at Kyoto, namely hydrofluorocarbons (HFCs), perfluorocarbons (PFCs) and sulphur hexafluoride (SF6), have very high GWPs but the quantities emitted to the atmosphere are far smaller than the emissions of CO2. Hence the contribution of these gases to global warming was equivalent to just 3% of the total contribution from CO2 emissions in 1995 (MCG, 1999). These are gases with particular industrial applications; HFCs and PFCs are substitutes for chlorofluorocarbons (CFC) and hydrochlorofluorocarbons (HCFC) which are being phased out under the Montreal Protocol because they deplete ozone levels in the stratosphere. A more detailed description of the usage, emissions and methodology for calculating emissions of these gases is given by MCG (1999).

The following sections present the inventories for each of the six greenhouse gases. To date, most international attention has focused on carbon dioxide and methane. Hence estimates of these pollutants were included in the UK inventory a number of years before the latter four pollutants. This is reflected in the longer time series of data available for carbon dioxide and methane. The overall accuracy of the inventories is also discussed. Full details of the methodology used to compile the inventory and the changes which have been made since the publication of the 1997 inventory are included in Appendices 1 and 3, respectively.