000280218 001__ 280218 000280218 005__ 20210129221240.0 000280218 0247_ $$2doi$$a10.1111/gcb.12686 000280218 0247_ $$2ISSN$$a1354-1013 000280218 0247_ $$2ISSN$$a1365-2486 000280218 0247_ $$2Handle$$a2128/9654 000280218 0247_ $$2WOS$$aWOS:000346698100009 000280218 0247_ $$2altmetric$$aaltmetric:2511631 000280218 0247_ $$2pmid$$apmid:25044767 000280218 037__ $$aFZJ-2016-00026 000280218 082__ $$a570 000280218 1001_ $$0P:(DE-HGF)0$$aBeringer, Jason$$b0$$eCorresponding author 000280218 245__ $$aFire in Australian savannas: from leaf to landscape 000280218 260__ $$aOxford [u.a.]$$bWiley-Blackwell$$c2015 000280218 3367_ $$0PUB:(DE-HGF)16$$2PUB:(DE-HGF)$$aJournal Article$$bjournal$$mjournal$$s1452497452_913 000280218 3367_ $$2DataCite$$aOutput Types/Journal article 000280218 3367_ $$00$$2EndNote$$aJournal Article 000280218 3367_ $$2BibTeX$$aARTICLE 000280218 3367_ $$2ORCID$$aJOURNAL_ARTICLE 000280218 3367_ $$2DRIVER$$aarticle 000280218 520__ $$aSavanna ecosystems comprise 22% of the global terrestrial surface and 25% of Australia (almost 1.9 million km2) and provide significant ecosystem services through carbon and water cycles and the maintenance of biodiversity. The current structure, composition and distribution of Australian savannas have coevolved with fire, yet remain driven by the dynamic constraints of their bioclimatic niche. Fire in Australian savannas influences both the biophysical and biogeochemical processes at multiple scales from leaf to landscape. Here, we present the latest emission estimates from Australian savanna biomass burning and their contribution to global greenhouse gas budgets. We then review our understanding of the impacts of fire on ecosystem function and local surface water and heat balances, which in turn influence regional climate. We show how savanna fires are coupled to the global climate through the carbon cycle and fire regimes. We present new research that climate change is likely to alter the structure and function of savannas through shifts in moisture availability and increases in atmospheric carbon dioxide, in turn altering fire regimes with further feedbacks to climate. 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