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Correction to Fire 2020, 3(2), 24.
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Correction

Correction: Hanes et al. Preceding Fall Drought Conditions and Overwinter Precipitation Effects on Spring Wildland Fire Activity in Canada. Fire 2020, 3, 24

by
Chelene Hanes
1,2,*,
Mike Wotton
1,2,
Douglas G. Woolford
3,
David L. Martell
1 and
Mike Flannigan
4
1
Graduate Department of Forestry, John H. Daniels Faculty of Architecture, Landscape and Design, University of Toronto, 33 Willcocks Street, Toronto, ON M5S 3B3, Canada
2
Great Lakes Forestry Centre, Canadian Forest Service, Natural Resources Canada, 1219 Queen St. E, Sault Ste. Marie, ON P6A 2E5, Canada
3
Statistical and Actuarial Sciences, University of Western Ontario, 1151 Richmond St., London, ON N6A 3K7, Canada
4
Department of Renewable Resources, University of Alberta, 51 General Services Building, Edmonton, AB T6G 2H1, Canada
*
Author to whom correspondence should be addressed.
Fire 2022, 5(5), 125; https://doi.org/10.3390/fire5050125
Submission received: 18 August 2022 / Accepted: 19 August 2022 / Published: 24 August 2022
(This article belongs to the Special Issue Boreal Fire-Fuels Interactions)
Browse Figure
Versions Notes
The authors wish to make the following corrections to this paper [1]:

Error in Figure

The authors found an error in Figure 3. The error is in one of the primary figures, which supports the interpretation of the results and conclusions. As it reads now, the figure shows the opposite results to those listed in the text.
The corrected Figure 3 appears below:
Fire 05 00125 g003 550
Figure 3. Examples of the resultant zero-inflated Poisson models for daily number of human-caused spring fires and FFMC (Fine Fuel Moisture Content) under low and high DCf values for (A) Grande Prairie and (B) Kirkland Lake. Values for low and high DCf are the same as those shown in Figure 2.
Figure 3. Examples of the resultant zero-inflated Poisson models for daily number of human-caused spring fires and FFMC (Fine Fuel Moisture Content) under low and high DCf values for (A) Grande Prairie and (B) Kirkland Lake. Values for low and high DCf are the same as those shown in Figure 2.
Fire 05 00125 g003
The authors apologize for any inconvenience caused and state that the scientific conclusions are unaffected. The original publication has also been updated.

Reference

  1. Hanes, C.; Wotton, M.; Woolford, D.G.; Martell, D.L.; Flannigan, M. Preceding Fall Drought Conditions and Overwinter Precipitation Effects on Spring Wildland Fire Activity in Canada. Fire 2020, 3, 24. [Google Scholar] [CrossRef]
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MDPI and ACS Style

Hanes, C.; Wotton, M.; Woolford, D.G.; Martell, D.L.; Flannigan, M. Correction: Hanes et al. Preceding Fall Drought Conditions and Overwinter Precipitation Effects on Spring Wildland Fire Activity in Canada. Fire 2020, 3, 24. Fire 2022, 5, 125. https://doi.org/10.3390/fire5050125

AMA Style

Hanes C, Wotton M, Woolford DG, Martell DL, Flannigan M. Correction: Hanes et al. Preceding Fall Drought Conditions and Overwinter Precipitation Effects on Spring Wildland Fire Activity in Canada. Fire 2020, 3, 24. Fire. 2022; 5(5):125. https://doi.org/10.3390/fire5050125

Chicago/Turabian Style

Hanes, Chelene, Mike Wotton, Douglas G. Woolford, David L. Martell, and Mike Flannigan. 2022. "Correction: Hanes et al. Preceding Fall Drought Conditions and Overwinter Precipitation Effects on Spring Wildland Fire Activity in Canada. Fire 2020, 3, 24" Fire 5, no. 5: 125. https://doi.org/10.3390/fire5050125

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