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Table 1.5.4<br />

Key categories under the Kyoto Protocol and corresponding categories under the<br />

Climate Change Convention<br />

Category as reported under the Climate Change<br />

Convention<br />

Conversion to Forest Land<br />

Conversion to Grassland<br />

Forest Land Remaining Forest Land<br />

Article 3.3 and 3.4 activities under the Kyoto<br />

Protocol<br />

Afforestation and reforestation<br />

Deforestation<br />

Forest Management<br />

1.6 Inventory uncertainty<br />

1.6.1 Reporting under the Climate Change Convention<br />

Uncertainty estimates are an essential element of a complete greenhouse gas emissions<br />

and removals Inventory. The purpose of uncertainty information is not to dispute the<br />

validity of the Inventory estimates but to help prioritise efforts to improve the accuracy of<br />

inventories and guide decisions on methodological choice (IPCC, 2006d). Inventories<br />

prepared in accordance with IPCC guidelines (IPCC, 2006d) will typically contain a wide<br />

range of emission estimates, varying from carefully measured and demonstrably complete<br />

data on emissions to order-of-magnitude estimates of highly variable emissions such as<br />

N 2 O fluxes from soils and waterways.<br />

In this Inventory submission, New Zealand included a Tier 1 uncertainty analysis of the<br />

aggregated figures as required by the Climate Change Convention Inventory guidelines<br />

(UNFCCC, <strong>2013</strong>) and IPCC good practice guidance (IPCC, 2006d). Uncertainties in the<br />

categories are combined to provide uncertainty estimates for the entire Inventory for the<br />

latest Inventory year and the uncertainty in the overall Inventory trend over time. LULUCF<br />

categories have been included using the absolute value of any removals of CO 2<br />

(table A2.1.1). Table A2.1.2 calculates the uncertainty in emissions only (ie, excluding<br />

LULUCF removals).<br />

In most instances, the uncertainty values are determined by analysis of emission factors<br />

or activity data using expert judgement from sectoral or industry experts, or by referring<br />

to uncertainty ranges provided in the IPCC guidelines. The uncertainty for CH 4 emissions<br />

from enteric fermentation was calculated by expressing the coefficient of variation<br />

according to the standard error of the methane yield. A Monte Carlo simulation has been<br />

used to determine uncertainty for N 2 O from agricultural soils. For the <strong>2013</strong> data, the<br />

uncertainty in the annual estimate was calculated using the 95 per cent confidence<br />

interval determined from the Monte Carlo simulation as a percentage of the mean value.<br />

Total emissions<br />

Uncertainty in <strong>2013</strong><br />

The uncertainty in total emissions (excluding emissions and removals from the<br />

LULUCF sector) is 13.1 per cent. This is a decrease of ± 0.2 per cent from 2012.<br />

Emissions of N 2 O from agricultural soils (section 6.5), CH 4 from enteric fermentation and<br />

CH 4 from solid waste disposal contribute the highest levels of uncertainty. These<br />

categories accounted for ± 7.7 per cent, ± 5.6 per cent and ± 8.6 per cent, respectively, of<br />

New Zealand’s total emissions uncertainty in <strong>2013</strong>. The uncertainty in these categories<br />

reflects the inherent variability when estimating emissions from natural systems.<br />

Uncertainty in the trend<br />

The trend uncertainty in total emissions (excluding emissions and removals from the<br />

LULUCF sector) from <strong>1990</strong> to <strong>2013</strong> is ± 14.6 per cent. This is an increase of ± 3.5 per<br />

New Zealand’s Greenhouse Gas Inventory <strong>1990</strong>–<strong>2013</strong> 21

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