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COMING ATTRACTIONS. CIG / JISAO PRESENTS. A GEDALOF, MANTUA, PETERSON PRODUCTION. A multi-century perspective of variability in the Pacific Decadal Oscillation: new insights from tree rings and coral. Reconstructed PDO Index. R = 0.64.
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CIG / JISAO PRESENTS A GEDALOF, MANTUA, PETERSON PRODUCTION
A multi-century perspective of variability in the Pacific Decadal Oscillation: new insights from tree rings and coral
Reconstructed PDO Index R = 0.64 • Based on leading principal component of five published paleoproxy reconstructions. • Collective skill better than individual skill
Mean Intercorrelation... Note Interval of Poor Intercorrelation
Linsley Evans Gedalof
COLUMBIA RIVER FLOW SINCE A.D. 1750 RECONSTRUCTED FROM TREE RINGS A Gedalof / Peterson / Mantua Joint
Based on 32 tree-ring sites R = 0.59
Residuals exhibit positive trend over time (ca. +1.2 percent per century) • Validates model results of Matheussen et al. (2000).
Persistent Droughts: • The 1930s were not an anomaly...
FIRE & CLIMATE IN THE AMERICAN NORTHWEST Douglas-Fir
CO-CONSPIRATORS Lolita (and Dave) Nate Ze’ev
Q. What causes wildfire? A. Fuels Accumulation "As with other areas of the country, we have experienced the unintended consequences of our very effective wildfire fighting program: The wildfires of today are getting bigger, more dangerous, harder to control, and are adversely affecting the safety of the public and our fire fighters.” National Fire Plan Strategy For the Pacific Northwest (2002)
Q. What causes wildfire? B. Weather "…forest fire behavior is determined primarily by weather variation among years rather than fuel variation associated with stand age." Bessie and Johnson (1995)
Q. What causes wildfire? C. You
Evidence for fuels... Area burned by wildfire in 11 Western States Source: National Interagency Fire Center
Cool PDO Warm PDO …for climate... On national forest lands in the Pacific Northwest wildfires are more frequent and more extensive during the warm phase of the PDO.
Study Overview • To characterize patterns in annual area burned • To relate those patterns to climatic features and ecological context • To determine the extent to which climatic factors can be used to predict seasonal wildfire
Literature Review • Lots of work in the Canadian boreal forest. • Very little work in the Pacific Northwest
Previous Studies • Have generally treated area west of the Rocky Mountains as a single coherent unit • No allowance for spatial variability • No recognition of underlying ecology • Emphasis has been on weather (not climate)
New Ideas: (1) I do not treat the area west of the Rocky Mountains as a single coherent unit (2) I address large fire seasons, rather than individual large fires (3) I identify several key atmospheric structures that can potentially be used to forecast fire-season severity
EOF Analysis • Empirical Orthogonal Function (EOF) analysis identifies underlying patterns in large data sets • The EOFs describe the spatial variability in the data set • Associated principal components (PCs) describe the temporal variability
Spatial Regressions • Can “regress” fields of climate data onto time series • Produces characteristic response of climate field to 1s perturbation in time series
Superposed Epoch Analysis • Develop map composites for selected years (i.e. epochs) based on quantitative criteria • Derive descriptive statistics for subsets • Can focus on extreme events • More powerful than correlations / regressions • Does not assume linear relationship
PC1 / 500 hPaRegression Shaded areas indicate significant correlation Pattern exhibits strong blocking
PC1 / 500 hPaComposite • Five largest fire years minus five smallest fire years • Patterns consistent, but magnitude greater
PC1 / PDSI Correlations Area burned is correlated to drought in winter and spring preceding the fire season Correlations: -0.59 -0.55 -0.61 June, July, Aug.
PC2 / 500 hPaRegression Resembles “Summer PNA” Matches results across border
PC2 / PDSI Correlations Area burned is weakly correlated to drought in winter preceding the fire season Correlations: -0.06 -0.09 -0.11 June, July, Aug.
PC3 / 500 hPaComposite • 3 only large fire years represented by PC-3 • Characterized by very strong, highly persistent blocking
Correlations Composite
PC4 / 500 hPaComposite • Large fire years correspond to fire season cyclone activity
Fire season is wet on the west side, dry on the east side Preceding season is drier than normal
Summary 1. Climate Matters • Region wide increases in area burned are characterized by antecedent drought accompanied by persistent blocking events
Summary 2. Ecology Matters • Underlying ecology appears to modulate the response to drought and circulation • more mesic forests require persistent drought, blocking events, and a source of ignition and spread • drier forests are more responsive to shorter-scale (i.e. synoptic) processes
Summary 3. These relationship are non-linear • Implies that eigenvector techniques may not be the most appropriate method of investigation • Small changes in mean climate may lead to dramatic changes in wildfire activity