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Climate and socioeconomic drivers of biomass burning and carbon emissions from fires in tropical dry forests: A Pantropical analysis

机译:热带干旱森林生物质燃烧和火灾碳排放的气候和社会经济驱动因素:泛热带分析

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Abstract Global burned area has declined by nearly one quarter between 1998 and 2015. Drylands contain a large proportion of these global fires but there are important differences within the drylands, for example, savannas and tropical dry forests (TDF). Savannas, a biome fire‐prone and fire‐adapted, have reduced the burned area, while the fire in the TDF is one of the most critical factors impacting biodiversity and carbon emissions. Moreover, under climate change scenarios TDF is expected to increase its current extent and raise the risk of fires. Despite regional and global scale effects, and the influence of this ecosystem on the global carbon cycle, little effort has been dedicated to studying the influence of climate (seasonality and extreme events) and socioeconomic conditions of fire regimen in TDF. Here we use the Global Fire Emissions Database and, climate and socioeconomic metrics to better understand long‐term factors explaining the variation in burned area and biomass in TDF at Pantropical scale. On average, fires affected 1.4 of the total TDF' area (60,208 km2) and burned 24.4 (259.6 Tg) of the global burned biomass annually at Pantropical scales. Climate modulators largely influence local and regional fire regimes. Inter‐annual variation in fire regime is shaped by El Niño and La Niña. During the El Niño and the forthcoming year of La Niña, there is an increment in extension (35.2 and 10.3) and carbon emissions (42.9 and 10.6). Socioeconomic indicators such as land‐management and population were modulators of the size of both, burned area and carbon emissions. Moreover, fires may reduce the capability to reach the target of “half protected species” in the globe, that is, high‐severity fires are recorded in ecoregions classified as nature could reach half protected. These observations may contribute to improving fire‐management.
机译:摘要 1998—2015年间,全球烧毁面积下降了近四分之一。旱地占全球火灾的很大一部分,但旱地内部存在重要差异,例如稀树草原和热带干旱森林(TDF)。热带草原是一个容易发生火灾且适应火灾的生物群落,减少了燃烧面积,而TDF的火灾是影响生物多样性和碳排放的最关键因素之一。此外,在气候变化情景下,预计TDF将增加其目前的范围并增加火灾风险。尽管存在区域和全球尺度的影响,以及该生态系统对全球碳循环的影响,但很少有人致力于研究气候(季节性和极端事件)和社会经济条件对TDF火灾方案的影响。在这里,我们使用全球火灾排放数据库以及气候和社会经济指标来更好地了解解释泛热带尺度上TDF燃烧面积和生物量变化的长期因素。在泛热带尺度上,火灾平均每年影响TDF总面积(60,208 km2)的1.4%,燃烧全球燃烧生物量的24.4%(259.6 Tg)。气候调节剂在很大程度上影响着当地和区域的火灾状况。厄尔尼诺现象和拉尼娜现象影响了火灾状况的年际变化。在厄尔尼诺现象和即将到来的拉尼娜现象期间,扩展(35.2%和10.3%)和碳排放量(42.9%和10.6%)有所增加。土地管理和人口等社会经济指标是烧毁面积和碳排放量的调节因素。此外,火灾可能会降低全球达到“半受保护物种”目标的能力,也就是说,在被归类为自然的生态区记录的高严重火灾可以达到一半受保护物种。这些观察结果可能有助于改善火灾管理。

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