International Journal of Wildland Fire International Journal of Wildland Fire Society
Journal of the International Association of Wildland Fire
RESEARCH ARTICLE

The relationship between the monsoonal summer rain and dry-season fire activity of northern Australia

S. Harris A D , N. Tapper A , D. Packham A , B. Orlove B C and N. Nicholls A

A School of Geography and Environmental Science, Monash University, Melbourne, VIC 3800, Australia.

B Department of Environmental Science and Policy, University of California, Davis, CA 95616, USA.

C Center for Research on Environmental Decisions, Columbia University, New York, NY 10027, USA.

D Corresponding author. Email: sarah.harris@arts.monash.edu.au

International Journal of Wildland Fire 17(5) 674-684 https://doi.org/10.1071/WF06160
Submitted: 6 December 2006  Accepted: 15 April 2008   Published: 3 October 2008

Abstract

Fire is an essential element of the northern Australian ecosystems with extensive areas burnt each year. The basic climate condition of high rainfall during the summer monsoon, followed by an extended warm dry winter, along with highly combustible vegetation (much of which grows rapidly during summer and senesces during winter), creates a highly flammable environment. These vegetation conditions change under various naturally occurring climate oscillations such as El Niño–Southern Oscillation (ENSO). The present paper investigates the link between burnt areas of northern Australia, rainfall, the Southern Oscillation Index (SOI) and sea surface temperatures (SST) for a 9-year period (1997–2005). The burnt area distribution is compared with the strength and timing of the monthly averaged rainfall, SOI and SST. Results indicate a strong relationship between antecedent rainfall and ENSO indices with area burnt. This is especially strong between the burnt areas of June–October and the preceding rainfall of November–March (r = 0.90), the SOI of November–February (r = 0.78) and the SST of June–August (r = –0.64). The results from the present study reveal the ability to forecast annual burnt areas and present some of the dynamics of the climate–fire interactions and their value for management systems.


Acknowledgements

SRSS of DLI for the mapped burnt areas of northern Australia. The Bureau of Meteorology for SOI and rainfall data from the software DIAGNOSE 3.0. The NWS of NOAA for the SST data. Three anonymous reviewers for their comments and suggestions.


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