Climate strongly influences the occurrence and extent of fires at the US West Coast and fire managers desire the ability to predict problematic fire seasons in advance> Currently, they must wait until the climatic pattern for the current year is well in place before the potential severtity of the coming fire season becomes apparent. Hemispheric-scale atmospheric circulation patterns (such as ENSO, PDO, and PNA), however, are predictable weeks to years in advance. The predictability of these patterns can thus potentially be used to predict fire season severity. In order to develop and evaluate this approach to predicting fire season severity, we identify the functional links between atmospheric circulation patterns, fire weather, and fire regimes over a range of spatial and temporal scales. The goal of this project is to identify the relationships of inter-annual and intra-decadal variation and multi-decadal and multi-century climate change on sub-regional variation in montane forest fire regimes in the Mediterranean Climate Area (MCA) of the Pacific Coast. Specific objectives are to:
The strength of this project are the wide range of spatial and temporal scales that are being covered. We investigate contemporary (1920-2000) fire-climate interactions using observational fire records from California, Oregon, Washington, and Nevada. Contemporary fire weather conditions (1960-2000) are studied on atmospheric scales as well as from local station data. Long-term (1700-1900) tree ring records of fire come from over 50 sites collected for this study extending from Baja California to Grants Pass, Oregon (see map). Over 1000 tree ring samples are analysed for this study.
This project was supported with funding from the National Forest Service and the Joint Fire Science Program