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Future changes in climatic water balance determine potential for transformational shifts in Australian fire regimes

Bibliographic Data

ID15545347
AuthorsMatthias M Boer (0000-0001-6362-4572, Western Sydney University, corresponding author), David M J S Bowman (0000-0001-8075-124X, University of Tasmania), Brett P Murphy (0000-0002-8230-3069, The University of Melbourne), Geoffrey J Cary (0000-0002-6386-1751, Australian National University), Mark A Cochrane (0000-0002-4573-568X, South Dakota State University), R J Fensham (0000-0003-3658-5867, The University of Queensland), Meg A Krawchuk (0000-0002-3240-3117, Simon Fraser University), Owen Price (0000-0001-5327-568X, University of Wollongong), Owen F Price, Víctor Resco de Dios (0000-0002-5721-1656, Western Sydney University), Richard J Williams (0000-0002-9558-9588, Commonwealth Scientific and Industrial Research Organisation), Ross A Bradstock (0000-0002-6904-2394, University of Wollongong)
Year2016
Volume11
Issue6
Pages065002-065002
Publication date2016-06-01
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueEnvironmental Research Letters (JOURNAL)
Journal identifiersISSN: 1748-9326 • E-ISSN: 1748-9326
PublisherIOP Publishing (PUBLISHER • GB)
DOI10.1088/1748-9326/11/6/065002
OpenAlexW2415843044
LanguageEN
Citations received8
References cited54

Most studies of climate change effects on fire regimes assume a gradual reorganization of pyrogeographic patterns and have not considered the potential for transformational changes in the climate-vegetation-fire relationships underlying continental-scale fire regimes. Here, we model current fire activity levels in Australia as a function of mean annual actual evapotranspiration (E) and potential evapotranspiration (E ), as proxies for fuel productivity and fuel drying potential. We distinguish two domains in space according to the dominant constraint on fire activity being either fuel productivity (PL-type fire) or fuel dryness (DL-type fire) and show that the affinity to these domains is related to fuel type. We propose to assess the potential for transformational shifts in fire type from the difference in the affinity to either domain under a baseline climate and projected future climate. Under the projected climate changes potential for a transformational shift from DL- to PL-type fire was predicted for mesic savanna woodland in the north and for eucalypt forests in coastal areas of the south-west and along the Continental Divide in the south-east of the continent. Potential for a shift from PL- to DL-type fire was predicted for a narrow zone of eucalypt savanna woodland in the north-east

Biology · Climate change · Climatology · Dryness · Ecosystem · Evapotranspiration · Fire regime · Grassland · Plant functional type · Productivity · Vegetation (pathology · Vegetation type · Woodland · Environmental Science · Fire effects on ecosystems · Plant Water Relations and Carbon Dynamics · Tree-ring climate responses · Ecology · Geology

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Unique citing works8
Citations per year0,89
Citation span2017 - 2025 (9)
Citation velocityrecent
Highly citedNo
Citation typesNeutral: 8
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