On the relationships between forest fires and weather conditions in Greece from longterm national observations ( )
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1 International Journal of Wildland Fire 2013, 22, IAWF 2013 Supplementary material On the relationships between forest fires and weather conditions in Greece from longterm national observations ( ) Nikos Koutsias A,F, Gavriil Xanthopoulos B, Dimitra Founda C, Fotios Xystrakis A, Foula Nioti A, Magdalini Pleniou A, Giorgos Mallinis D and Margarita Arianoutsou E A Department of Environmental and Natural Resources Management, University of Ioannina, G. Seferi 2, GR Agrinio, Greece. B Hellenic Agricultural Organisation Demeter, Institute of Mediterranean Forest Ecosystems and Forest Products Technology, PO Box 14180, Terma Alkmanos, Ilisia, GR Athens, Greece. C Institute for Environmental Research and Sustainable Development, National Observatory of Athens. D Department of Forestry & Management of the Environment and Natural Resources, Democritus University of Thrace, Pantazidou 193, GR Orestiada, Greece. E Department of Ecology & Systematics, Faculty of Biology, National & Kapodistrian University of Athens, Panepistimiopolis Ilisia, GR Athens, Greece. F Corresponding author. nkoutsia@cc.uoi.gr Table S1. Generalised least squares (GLS) regression outputs Residual autocorrelation has not been taken into account. Abbreviations as in Table 4 Coefficients GLS regression (without residual fit) Value s.e. t-value P (Intercept) * T max mean ** T max abs * p fir ** Model diagnostics AIC BIC loglik Standardised residuals Min. Q1 Med. Q3 Max Residual standard error: Page 1 of 5
2 Fig. S1. Autocorrelation function (ACF) diagrams for the historical data of fire records (number of fires and area burned) in Greece for the periods (left column) and (right column). Dashed lines indicate the 95% confidence intervals estimated by means of the Bartlett equation (Hipel and McLeod 1994). Page 2 of 5
3 Fig. S2. Autocorrelation function (ACF) diagrams for the historical meteorological data in Greece for the periods (first two columns) and (last two columns). Dashed lines indicate the 95% confidence intervals estimated by means of the Bartlett equation (Hipel and McLeod 1994). Page 3 of 5
4 Tmean - Burned area ( ) pwin - Burned area ( ) Tmean - Burned area ( ) pwin - Burned area ( ) Tmax mean - Burned area ( ) pspr - Burned area ( ) Tmax mean - Burned area ( ) pspr - Burned area ( ) Tmax abs - Burned area ( ) psum - Burned area ( ) Tmax abs - Burned area ( ) psum - Burned area ( ) Tmin mean - Burned area ( ) paut - Burned area ( ) Tmin mean - Burned area ( ) paut - Burned area ( ) ptot - Burned area ( ) pfir - Burned area ( ) ptot - Burned area ( ) pfir - Burned area ( ) Fig. S3. Cross-correlation function () graphs between corrected area burned and selected temperature and precipitation parameters in Greece for the periods (first two columns) and (last two columns) Dashed lines indicate the 95% confidence intervals. Abbreviations: T mean, mean annual air temperature; T max, maximum air temperature; T min, minimum air temperature; p tot, total annual precipitation; p win, winter precipitation; p spr, spring precipitation; p sum, summer precipitation; p aut, autumn precipitation; pfir, fire season precipitation. Page 4 of 5
5 Fig. S4. Standardised regression residuals. Autocorrelation (ACF) and partial autocorrelation function (PACF) diagrams (left) and histogram and QQplot of standardised residuals of generalised least squares (GLS) regression without autoregressive moving average (ARMA) fit to residuals (right). References Hipel KW, McLeod AI (1994) Time Series Modelling of Water Resources and Environmental Systems. (Elsevier: Amsterdam, the Netherlands) Page 5 of 5
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