Fire Cycle East Fraser Sample Clauses

Fire Cycle East Fraser. For the purposes of calculating a fire interval, the period of reliability is considered to be 1961-1869. Based on this 92 year period of record, a fire cycle of 98.9 years is calculated, when fire overlap is not accounted for (Xxxxxxx et al., 2002, pg 116). Xxxxxxx et al. states that this method has been used by previous researchers (Xxxx 1990), and (Wien 1977). When the adjusted time since fire distribution is used with the inclusion of the 1/3 fire overlap ‘rule of thumb’, an approximate fire cycle of 60 years is calculated (Xxxxxxx et al., 2002 pg 117). However, Xxxxxxx et al. goes on to state that interpretation of the TSF age distribution in the context of individual burn patterns suggests a burn cycle of 50-90 years. Xxxxxx (2002) used a fire cycle of 100 years for age class distribution and seral stage distribution based on local data, or from adjacent landscapes that were felt to have a similar disturbance history which had study information. The natural disturbance unit that Xxxxxx used the 100 year fire return interval for is termed the Moist Interior – Plateau, and includes several of the same biogeoclimatic zones and subzones that are within the East Fraser study area. Andison (1996), in the Prince Xxxxxx Region SBS biogeoclimatic zone calculated a mean fire interval of 80-100 years for stand replacing fires using forest cover maps with ground truthing to further separate age class 8 and 9 stands into 20 year classes. Xxxxxxx et al. 2002 (pg 117) states that based on the similarity of the TSF age class distributions, the fire cycle appears to be similar for all the major subzones in the east Fraser study area. A slightly longer fire cycle would be found for the wetter southeastern portion of the study area.
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