2016
DOI: 10.1007/s11676-016-0235-0
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Analysis of the forest fires in the Antalya region of Turkey using the Keetch–Byram drought index

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Cited by 10 publications
(5 citation statements)
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“…When these results are assessed on the basis of countries, the explained variance is lower because large fires occur intensely in some regions like in Turkey. While a strong relationship between the amount of burned areas and FWI, BUI, ISI and SSR values in Balıkesir region was stated by Ertuğrul and Varol [6], in Muğla region was found a relationship only between SSR and the amount of burned area. Similarly, the regression equation found by Balshi et al [59] for the west of Canada explains 80% of the variance, whereas the one for the east of Canada is able to explain only 43% of the variance.…”
Section: Resultsmentioning
confidence: 90%
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“…When these results are assessed on the basis of countries, the explained variance is lower because large fires occur intensely in some regions like in Turkey. While a strong relationship between the amount of burned areas and FWI, BUI, ISI and SSR values in Balıkesir region was stated by Ertuğrul and Varol [6], in Muğla region was found a relationship only between SSR and the amount of burned area. Similarly, the regression equation found by Balshi et al [59] for the west of Canada explains 80% of the variance, whereas the one for the east of Canada is able to explain only 43% of the variance.…”
Section: Resultsmentioning
confidence: 90%
“…Normal or extreme values of KBDI and SPEI could not take place in the equations obtained as a result of step-wise regression. In a study in Antalya carried out by Varol and Ertuğrul [6], it was found that there was a significant relationship between KBDI values and the burned area only in the years when big fires arose but there was no relationship between KBDI values and the number of fires. As a result of step-wise regression analysis, the extreme ones of FWI, DSR, T components for both the burned area and the number of fires were selected as significant variables.…”
Section: Resultsmentioning
confidence: 98%
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“…The low-NDVI grid cells identified in this study typically represented summers with a heat-and/or drought-induced loss of forest greenness (Anyamba and Tucker, 2012;Orth et al, 2016;Buras et al, 2020). Known drought and heat events were identified as low-NDVI events, e.g., the Iberian drought in 2005 (Gouveia et al, 2009), a 2-year-long drought in 2007-2008 in Turkey (Varol and Ertugrul, 2016), the 2011-2013 drought in the Balkans (Cindrić et al, 2016), the hot summer of 2017 in Italy (Rita et al, 2020), and the central European hot drought in 2018 (Schuldt et al, 2020;Senf and Seidl, 2021b). Additionally, we identify 2022 as a recordbreaking year of the most widespread low-NDVI events covering 37 % of the Mediterranean and temperate forest biome each.…”
Section: Low-ndvi Eventsmentioning
confidence: 94%
“…As proxies for biophysical factors we used topographic characteristics of the terrain-slope, elevation, and aspect-which are proved to be important factors for the outbreak and prediction of fire (Maingi and Henry 2007;Dlamini 2010). For climate proxies we used average annual precipitation (since its reduction can lead to more frequent and longer droughts), average annual temperature (as the air temperature has a high correlation with the frequency of wildfires and areas affected by the fire), and forest aridity index (since intensification and the number of fires are linked to drought and aridity) (Alencar et al 2015;MPZS 2015;Varol and Ertugrul 2016).…”
Section: Datamentioning
confidence: 99%