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Climate change is playing an increasing role in determining wildfire regimes alongside human activity (medium confidence), with future climate variability expected to enhance the risk and severity of wildfires in many biomes such as tropical rainforests (high confidence). Fire weather seasons have lengthened globally between 1979 and 2013 (low confidence). Global land area burned has declined in recent decades, mainly due to less burning in grasslands and savannahs (high confidence). While drought remains the dominant driver of fire emissions, there has recently been increased fire activity in some tropical and temperate regions during normal to wetter than average years due to warmer temperatures that increase vegetation flammability (medium confidence). The boreal zone is also experiencing larger and more frequent fires, and this may increase under a warmer climate (medium confidence). Cross-Chapter Box 4 in this chapter
However, climate is only one driver of a complex set of environmental, ecological and human factors in influencing fire regimes (Bowman et al. 2011485). While these factors lead to complex projections of future burnt area and fire emissions (Knorr et al. 2016a486, b487), human exposure to wildland fires could still increase due to population expansion into areas already under high risk of fires (Knorr et al. 2016a488, b489). There are still major challenges in projecting future fire regimes and how climate, vegetation and socio/economic factors will interact (Hantson et al. 2016490; Harris et al. 2016491). There is also need for integrating various fire management strategies, such as fuel-reduction treatments in natural and planted forests, with other environmental and societal considerations to achieve the goals of carbon emissions reductions, maintain water quality, biodiversity conservation and human safety (Moritz et al. 2014492; Gharun et al. 2017493).
In summary, climate change is playing an increasing role in determining wildfire regimes alongside human activity (medium confidence), with future climate variability expected to enhance the risk and severity of wildfires in many biomes, such as tropical rainforests (high confidence). Fire weather seasons have lengthened globally between 1979 and 2013 (low confidence). Global land area burned has declined in recent decades, mainly due to less burning in grasslands and savannas (high confidence). While drought remains the dominant driver of fire emissions, there has recently been increased fire activity in some tropical and temperate regions during normal to wetter-than-average years due to warmer temperatures that increase vegetation flammability (medium confidence). The boreal zone is also experiencing larger and more frequent fires, and this may increase under a warmer climate (medium confidence).
With respect to atmospheric CH4 growth rates, we conclude that there is significant and ongoing accumulation of CH4 in the atmosphere (very high confidence). The reason for the pause in growth rates and subsequent renewed growth is at least partially associated with land use and land use change. Evidence that variation in the atmospheric OH sink plays a role in the year-to-year variation of the CH4 is accumulating, but results are contradictory (medium evidence, low agreement) and refining this evidence is constrained by lack of long-term isotopic measurements at remote sites, particularly in the tropics. Fugitive emissions likely contribute to the renewed growth after 2006 (medium evidence, high agreement). Additionally, the recent depletion trend of 13C isotope in the atmosphere indicates that growth in biogenic sources explains part of the current growth and that biogenic sources make up a larger proportion of the source mix compared to the period before 1997 (robust evidence, high agreement). In agreement with the findings of AR5, we conclude that wetlands are important drivers of inter- annual variability and current growth rates (medium evidence, high agreement). Ruminants and the expansion of rice cultivation are also important contributors to the current growth trend (medium evidence, high agreement).
While the rising atmospheric concentration of GHGs is the largest driver of anthropogenic changes in climate, the levels of short-lived climate forcers (SLCF) can significantly modulate regional climate by altering radiation exchanges and hydrological cycle and impact ecosystems (high confidence) (Boucher et al. 2013793; Rogelj et al. 2014794; Kok et al. 2018795). This section assesses the current state of knowledge with respect to past and future emissions of the three major SLCFs and their precursors: mineral dust, carbonaceous aerosols (black carbon (BC) and organic carbon (OC)) and BVOCs. This section also reports on implications of changes in their emissions for climate. Aerosols particles with diameters between about 0.010 μm to about 20 μm are recognised as SLCFs, a term that refers to their short atmospheric lifetime (a few days). BVOCs are important precursors of ozone and OC, both important climate forcing agents with short atmospheric lifetimes.
OC is also characterised by a high solubility with a high fraction of water-soluble organic compounds (WSOC) and it is one of the main drivers of the oxidative potential of atmospheric particles. This makes particles loaded with oxidised OC an efficient cloud condensation nuclei (CCN) in most of the conditions (Pöhlker et al. 2016852; Thalman et al. 2017853; Schmale et al. 2018854).
Consuming locally produced food and enhancing the efficiency of food processing and transportation can minimise food losses, contribute to food security and, in some circumstances, reduce GHG emissions (Brodt et al. 20131479; Michalský and Hooda 20151480; Tobarra et al. 20181481) (Section 5.5.2.3). Furthermore, urban agriculture has the potential to counteract the separation of urban populations from food production. This separation is one driver of the transition towards more homogeneous, high-protein diets, which are associated with increased GHG emissions (Goldstein et al. 20171482; Moragues-Faus and Marceau 20181483; Magarini and Calori 20151484). Barriers to the uptake of urban agriculture as a climate change mitigation option include the need for efficient distribution systems to ensure lowered carbon emissions (Newman et al. 20121485) and the concern that urban agriculture may harbour pathogenic diseases, or that its products be contaminated by soil or air pollution (Hamilton et al. 20141486; Ercilla-Montserrat et al. 20181487). 2ff7e9595c
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