Managing fire regimes in north Australia J Russell-Smith et al. ). Conversely, very limited burning is typically undertaken in more fertile, productive settings, despite the potential for applying relatively intense fires to combat encroachment by woody vegetation in some pastoral regions (Williams et al. 2002).Much of the frequently fire-affected land is under Aboriginal ownership -either under freehold title or, increasingly, under non-exclusive title arrangements (known as "native title"), as part of recent formal Australian State and Territory Government recognition of prior Aboriginal custodianship. Outside of urban settlements, Aboriginal people constitute the majority of the rural population in remote north Australian territories and, despite being "land rich", they remain severely economically and socially disadvantaged (RussellSmith et al. 2009b; White-head et al. 2009).Fires are deliberately ignited for a variety of traditional Aboriginal and other landmanagement purposes; lightning ignitions are confined to the onset of the stormy monsoonal season, typically between October and December (Russell-Smith et al. 2007). Minimal infrastructure combined with a very sparsely settled rural population (< 0.1 person per km 2 ) has resulted in a limited capacity to manage escaped fires; fire regimes in many regional settings are therefore characterized by the frequent (annual-biennial) recurrence of large (> 1000 km 2 ), late dryseason wildfires. Despite the appearance that relatively unmodified north Australian, eucalypt-dominated savanna systems are structurally intact and healthy, contemporary fire regimes are increasingly recognized as having drastic regional impacts on sustainable land use (Russell-Smith et al. 2003b), biodiversity (Woinarski et al. 2011;Russell-Smith et al. 2012), and GHG emissions and C storage (Murphy et al. 2010;Williams et al. 2012). The development of these contemporary burning patterns follows a breakdown in traditional Aboriginal methods of fire management, associated with societal collapse dating from the late 19th century (Ritchie 2009;. Traditionally, burning was undertaken throughout the year over much of northern Australia, with a focus on implementing extensive "cleaning of country" management through intensive application of small patchy burns in the early-mid dry season (Russell-Smith et al. 2003b). In Aboriginal-owned West Arnhem Land, for 2010). Typically, accountable GHG emissions contribute between 2-4% of Australia's annual National Greenhouse Gas Inventory (NGGI; ANGA 2011a). In accordance with international accounting rules, Australia's NGGI does not account for carbon dioxide (CO 2 ) emissions from savanna burning, on the assumption that such fires produce no net CO 2 flux (IPCC 1997). However, it is recognized that C fluxes in flammable savanna systems are dependent on fire regime characteristics, especially under changing fire frequency and intensity conditions (Beringer et al. 2007;Cook and Meyer 2009).In accordance with other provisions of the Kyoto Protocol, ...