Evaluating the Drought Code for lowland taiga of Interior Alaska using eddy covariance measurements
Eric A. Miller A * , Hiroki Iwata B , Masahito Ueyama C , Yoshinobu Harazono D , Hideki Kobayashi E , Hiroki Ikawa F , Robert Busey G , Go Iwahana G and Eugénie S. Euskirchen HA Bureau of Land Management, Alaska Fire Service, Fort Wainwright, AK, USA.
B Department of Environmental Science, Shinshu University, Matsumoto, Nagano, Japan.
C Graduate School of Agriculture, Osaka Metropolitan University, 1-1 Gakuen-cho, Naka-ku, Sakai, Osaka 599-8531, Japan.
D Graduate School of Life and Environmental Sciences, Osaka Prefecture University, Sakai, Osaka, Japan.
E Japan Agency for Marine-Earth Science and Technology, 3173-25 Showamachi, Kanazawa-ku, Yokohama, Kanagawa, 236-0001, Japan.
F Hokkaido Agricultural Research Center, National Agriculture and Food Research Organization, Hitsujigaoka, Toyohira Ward, Sapporo, Hokkaido, 062-8555, Japan.
G International Arctic Research Center, University of Alaska Fairbanks, Fairbanks, AK, USA.
H Institute of Arctic Biology, University of Alaska Fairbanks, Fairbanks, AK, USA.
International Journal of Wildland Fire 32(8) 1226-1243 https://doi.org/10.1071/WF22165
Submitted: 20 July 2022 Accepted: 19 May 2023 Published: 30 June 2023
© 2023 The Author(s) (or their employer(s)). Published by CSIRO Publishing on behalf of IAWF. This is an open access article distributed under the Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License (CC BY-NC-ND)
Abstract
Background: The Drought Code (DC) of the Canadian Fire Weather Index System (CFWIS) has been intuitively regarded by fire managers in Alaska, USA, as poorly representing the moisture content in the forest floor in lowland taiga forests on permafrost soils.
Aims: The aim of this study was to evaluate the DC using its own framework of water balance as cumulative additions of daily precipitation and substractions of actual evaporation.
Methods: We used eddy covariance measurements (EC) from three flux towers in Interior Alaska as a benchmark of natural evaporation.
Key results: The DC water balance model overpredicted drought for all 14 site-years that we analysed. Errors in water balance cumulated to 109 mm by the end of the season, which was 54% of the soil water storage capacity of the DC model. Median daily water balance was 6.3 times lower than that measured by EC.
Conclusions: About half the error in the model was due to correction of precipitation for canopy effects. The other half was due to dependence of the actual evaporation rate on the proportional ‘fullness’ of soil water storage in the DC model.
Implications: Fire danger situational awareness is improved by ignoring the DC in the CFWIS for boreal forests occurring on permafrost.
Keywords: Canadian Fire Weather Index System, duff moisture content, energy flux, evaporation, fire danger rating, permafrost, Picia mariana, wildfire.
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