Sierra Nevada fire severity conclusions are robust to further analysis: a reply to Safford et al.
Chad T. Hanson A D and Dennis C. Odion B CA Earth Island Institute, 2150 Allston Way, Suite no. 460, Berkeley, CA 94704, USA.
B Earth Research Institute, University of California, Santa Barbara, CA 93106, USA.
C Environmental Studies Department, Southern Oregon University, Ashland, OR 97520, USA.
D Corresponding author. Email: cthanson1@gmail.com
International Journal of Wildland Fire 24(2) 294-295 https://doi.org/10.1071/WF14219
Submitted: 12 December 2014 Accepted: 29 January 2015 Published: 10 March 2015
Abstract
Safford et al. (this issue) question our earlier findings that fire severity has not increased in Sierra Nevada conifer forests 1984–2010, hypothesising that an increasing trend might have appeared had we restricted our analysis to wildland fire in frequent-fire forest types on US Forest Service lands. Here, we tested that hypothesis and again found no trend of increasing severity.
Safford et al. (this issue) question our finding in IJWF, in Hanson and Odion (2014) (‘H&O’), that fire severity has not increased in Sierra Nevada forests. Safford et al. (‘SMC’) suggest that our inclusion of national park and private lands, prescribed burns and forest types with relatively infrequent fire regimes (e.g. lodgepole pine (Pinus contorta) and red fir (Abies magnifica)) could potentially have influenced our findings, and that restricting the analysis to US Forest Service lands, and forest types with frequent fire regimes (mixed-conifer, ponderosa pine (Pinus ponderosa) and Jeffrey pine (Pinus jeffreyi)), might have resulted in an increasing trend in high-severity fire 1984–2010. We note, initially, that Miller et al. (2009), Miller and Safford (2012) and Mallek et al. (2013), cited by SMC, all included national park lands and private lands (e.g. ~20% of fires were on private lands in Miller et al. 2009 (tables 1 and 2), almost identical to the amount in H&O), and prescribed fires comprised a negligible 0.15% of the high-severity fire analysed in H&O. Although we believe inclusion of all land ownerships is appropriate, as our purpose in H&O was to investigate patterns across the whole landscape, the points raised by SMC are worthy of evaluation and we appreciate that SMC brought them to our attention. In that spirit, we tested the approach promoted by SMC, and re-analysed our data for 1984–2010, using the methods described in H&O, but with the analysis restricted to wildland fires in mixed-conifer, ponderosa pine and Jeffrey pine forests on US Forest Service lands. We found no trend in high-severity fire area (z = 1.00, P = 0.317) or proportion (z = 0.47, P = 0.638).
Second, SMC suggest that the Mann–Kendall (M-K) non-parametric trend test we used has ‘very low’ statistical power relative to parametric tests they previously used, citing Helsel and Hirsch (2002), Yue et al. (2002) and Dickson et al. (2005). However, SMC do not accurately characterise these sources. Yue et al. (2002, fig. 8) specifically found that, with non-parametric data (SMC and H&O agree the Sierran fire severity data are non-parametric), the M-K test has much higher statistical power than parametric tests (see also Önöz and Bayazit 2003). Helsel and Hirsch (2002) concluded that M-K performs ‘either as well or better’ than parametric tests for non-normal data. Wiedemeier et al. (2005) (cited by SMC as Dickson et al. 2005) did not conclude findings of no trend with M-K are ‘usually a statement that the available data are not sufficient to discern a trend’, as SMC state. Rather, Wiedemeier et al. (2005) merely articulated a statistical tautology that weak patterns may not appear when data are very poor or insufficient, which is not the case for our 27-year analysis. Indeed, Wiedemeier et al. (2005) recommend use of M-K, and call it ‘robust’.
Third, SMC note the post-time-series vegetation data used in Miller et al. (2009), Miller and Safford (2012) and Mallek et al. (2013) are based on ‘potential’ vegetation, hypothesising that conifer forest would not be remapped as non-conifer after high-severity fire. This is a reasonable hypothesis. However, in H&O, we investigated this question and found that, in fact, areas mapped as conifer forest in these potential vegetation datasets are, as a matter of actual practice, frequently remapped as non-conifer vegetation (mostly shrub) years after high-severity fire. Our quantitative analysis in H&O found that this effect occurs to a disproportionate, and statistically significant, degree in the earlier years of the time series, causing relatively more high-severity fire in conifer forest to be excluded in the earlier years than in more recent years, and leading to the appearance of an increasing trend in fire severity even if none actually exists.
The foregoing addresses the major issues raised by SMC. We address what we view as less central, but not unimportant, criticisms raised by SMC in Table 1.
Recent studies have found that current rates of high-severity fire, including in frequent-fire forest types, are often substantially lower than historical rates (Odion and Hanson 2013; Baker 2014; Odion et al. 2014; Hanson and Odion in press). This raises a conservation concern for the many rare and declining wildlife species positively associated with the unique, and highly biodiverse, habitat created by high-severity fire: ‘complex early seral forest’ – particularly given frequent post-fire logging of this habitat (DellaSala et al. 2014; Hanson 2014). This broader ecological context is relevant to evaluations of fire patterns and trends.
Acknowledgements
Thanks are due to Tim Sinnott of GreenInfo Network for the geographic information systems (GIS) layering.
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