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ghg-inventory-1990-2013

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with the clearing of vegetation prior to the establishment of exotic planted forest. Belowground<br />

biomass is assumed not to burn. The IPCC default combustion proportion for the<br />

burning of non-eucalypt temperate forest in land clearing fires (0.51) is then applied to<br />

estimate emissions from this activity (Wakelin, 2012).<br />

The survey also provided data on the burning of post-harvest slash prior to restocking.<br />

This activity was found to occur mainly as a training exercise for wildfire control or for<br />

the clearing of slash heaps on skid sites. The data indicated that 0.8 per cent of<br />

restocked area was burnt each year in recent years. This estimate was combined with two<br />

earlier estimates of controlled burning in planted forest (Forest Industry Training and<br />

Education Council, 2005; Robertson, 1998) to provide activity data throughout the time<br />

series. It is assumed that 1.6 per cent of restocked area was burnt from <strong>1990</strong> to 1997.<br />

From 1997, the area burnt declines linearly to 0.8 per cent, which is used from 2005<br />

onwards (Wakelin, 2012).<br />

Activity data is combined with an emission factor derived from the pre-<strong>1990</strong> planted<br />

forest carbon-yield table to estimate emissions from the burning of post-harvest slash<br />

(harvest residue) on Forest land. The harvest residue is calculated by subtracting the<br />

amount of above-ground biomass that is taken off site as logs (70 per cent) from the total<br />

above-ground biomass predicted at the age of 28 years (the average harvest age in<br />

New Zealand). Below-ground biomass is assumed not to burn. The IPCC default<br />

combustion proportion for the burning of harvest residue in non-eucalypt temperate forest<br />

(0.62) is applied to estimate emissions from this activity (Wakelin, 2012).<br />

An estimate is provided for burning of post-harvest residues associated with deforestation<br />

in the Inventory. No information is available on the extent of burning associated with<br />

deforestation in New Zealand. Therefore, it is assumed that 30 per cent of conversions<br />

involve burning to clear residues. The IPCC default combustion proportion for the<br />

burning of harvest residue in non-eucalypt temperate forest (0.62) is applied to<br />

subcategory-specific emission factors to estimate emissions from this activity. The<br />

emission factor excludes the proportion of logs taken off site (70 per cent of aboveground<br />

biomass) and is taken from the plot-network-derived yield tables by forest<br />

subclass at the average age of harvest in New Zealand.<br />

Carbon dioxide emissions from controlled burning in planted forests in the Inventory are<br />

captured at the time of conversion or harvest.<br />

Different emission factors derived from the LUCAS plot network are used for wildfire<br />

and controlled burning on grassland with woody biomass in the Inventory.<br />

The differences are due to the vegetation that is typically converted to forest, which is<br />

generally of a lesser stature when compared with other shrubland (Wakelin and<br />

Beets, <strong>2013</strong>).<br />

Uncertainties and time-series consistency<br />

Uncertainties arise from relatively coarse activity data for wildfires and controlled<br />

burning activities in New Zealand (table 6.11.3). The biomass burning statistics have gaps<br />

in the time series where data collection did not occur or survey methodologies changed.<br />

Assumptions are made for some activity data, emission factors and burning fractions<br />

where insufficient data exists.<br />

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

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