A Synoptic Climatology for Forest-Fires in the NE US and Future Implications From GCM Simulations

We studied surface-pressure patterns corresponding to reduced precipitation, high evaporation potential, and enhanced forest-fire danger for West Virginia, which experienced extensive forest-fire damage in November 1987. From five years of daily weather maps we identified eight weather patterns that describe distinctive flow situations throughout the year. Map patterns labeled extended-high, back-of-high, and pre-high were the most frequently occurring patterns that accompany forest fires in West Virginia and the nearby four-stare region. Of these, back-of-high accounted for a disproportionately large amount of fire-related damage. Examination of evaporation acid precipitation data showed that these three patterns and high-to-the-south patterns ail led to drying conditions and all other patterns led to moistening conditions. Surface-pressure fields generated by the Canadian Climate Centre global circulation model for simulations of the present (1xCO 2 ) climate and 2xCO 2 climate were studied to determine whether forest-fire potential would change under increased atmospheric CO 2 . The analysis showed a tendency for increased frequency of drying in the NE US, but the results were not statistically significant. International Journal of Wildland Fire 4(4) 217 - 224 Full text doi:10.1071/WF9940217 © CSIRO 1994