“
“Peat deposits in temperate regions represent a significant global carbon sink. Estimates of stocks in Great Britain vary fairly wildly from ca. 3 Gt (Cannell et al., 1993 and Worrall et al., 2011) for the whole region to between 4.5 Gt (Milne and Brown, 1997) and 16 Gt (Howard et al., 1995) for Scotland alone. In the UK the use of management fire on peatlands is controversial because

good evidence of the long-term effects of management (e.g. burning, grazing, drainage and afforestation) on the ecology, hydrology and carbon balance of peatlands is lacking (Birkin et al., 2011 and Worrall et al., 2011). Nevertheless the immediate impacts of severe wildfires are likely to be much more apparent than the gradual changes caused by land management. Severe fires in peatlands

can lead to the ignition of peat deposits and extensive smouldering combustion particularly following periods of extended drought MK-8776 order or where peat structure and moisture have been altered by drainage and/or afforestation. Peat fires are dominated by smouldering which is the slow, low temperature (peak ∼ 600 °C), flameless combustion of organic matter (Rein et al., 2008 and Hadden et al., 2013). This is the most persistent type of combustion and exhibits fire behaviour drastically different from flaming wildfires (Rein, 2013). Peat megafires have been identified as the largest fires on Earth in terms of fuel consumption and can burn up to 100 times more fuel per unit area than learn more flaming fires (Rein, 2013). Wildfires that ignite peat require considerable resources to control and can have impacts that last decades if not centuries (e.g. Legg et al., 1992). Peat fires can also release significant amounts of stored carbon (Maltby et al., 1990 and Page et al., 2002) and, with climate predictions forecasting increased fire risk across a number of areas that hold substantial peat deposits (Flannigan et al., 2009, Krawchuk et al., 2009 and Jenkins et al., 2010), they may represent

an important positive feedback on the atmospheric radiative forcing that exerts a controlling influence Phospholipase D1 on climate warming (Field et al., 2007 and Rein, 2013). Many countries have pledged to reduce carbon emissions by 2050, however, current emission estimates, for example in the UK, do not take into account those from peatlands (Bain et al., 2012). This is because there is still considerable uncertainty as to whether peatlands represent a net carbon source or sink (Worrall et al., 2011), the reporting of peatland emissions is currently voluntary under Article 3.4 of the Kyoto Protocol, and reporting is only considered for wetland drainage and rewetting (Bain et al., 2012). In addition there is little evidence for the long or short term effects of wildfires on carbon emissions from peatlands despite the global importance of fire in these systems (e.g. Turetsky et al., 2002 and Couwenberg et al.