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Supplementary Material
Evidence of a historical frequent, low-severity fire regime in western Washington, USA
Jonathan D. Bakker1*, Ellen Jones1, and Carson B. Sprenger2
1 School of Environmental and Forest Sciences, University of Washington, Box 354115, Seattle,
WA 98195-4115, USA; E: [email protected]
2 Rain Shadow Consulting LLC, P.O. Box 1776, Eastsound, WA 98245, USA
* Corresponding author.
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Figure S1. Aerial photographs of the Kellett Bluff (top) and Turn Point (bottom) sites in 1965
(left) and 2001 (right). The 1965 photos are from Pacific Aerial Surveys, and the 2001 photos
are from the Washington Department of Natural Resources. Scale is not shown, but differs
between sites.
Figure 2. Aerial photographs of the Kellett Bluff (top) and Turn Point (bottom) sites in 1965 (left) and 2001 (right). The 1965 photos are from Pacific Aerial Surveys, and the 2001 photos are from the Washington Department of Natural Resources. Scale is not shown, but differs between sites.
1965 2001
1965 2001
Turn
Poi
ntK
elle
tt B
luff
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Figure S2. Standardized ring width index (RWI) from 1650-2011, based on 16 Douglas-fir trees
at Kellett Bluff. The dark grey line shows the annual ring width indices, and the red line shows a
running average. The grey polygon behind the lines shows the sample depth. Raw ring widths
are available through the International Tree Ring Databank
(https://www.ncdc.noaa.gov/paleo/study/26250).
Figure A1. Ring width indices from 1650-2011. The dark grey line shows the annual ring width indices, and the red line shows a running average. The grey polygon behind the lines shows the sample size.
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Table S1. Details of samples obtained from the Kellett Bluff (WKB) site, San Juan Islands,
Washington. Fire history data are available through the International Multiproxy Paleofire
Database (https://www.ncdc.noaa.gov/paleo/study/26331).
Site Sample
Number
Live? Full or
Partial?
Crossdated? Notes
WKB 8 Yes Partial No
WKB 9 No Full Yes Was WKB 7? rotten
WKB 11 Yes Partial No
WKB 15 Yes Partial No 2 pieces
WKB 20 No Full Yes Rotten
WKB 21 Yes Partial Yes 2 pieces
WKB 22 No Partial Yes
WKB 54 Yes Partial No
WKB 58 Yes Partial Yes
WKB 59 Yes Partial Yes 3 pieces
WKB 61 No Full Yes
WKB 62 No Full Yes Rotten
WKB 64 No Full Yes 2 samples
WKB 65 No Full Yes 2 samples; no bark
WKB 66 No Full Yes No sign of cambium
WKB 67 Yes Partial Yes 2 samples (3 pieces)
WKB 69 No Full Yes No bark
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Site Sample
Number
Live? Full or
Partial?
Crossdated? Notes
WKB 71 No Full Yes Hollow
WKB 72 Yes Partial Yes 3 pieces
WKB Total 19 Yes: 9
No: 10
Partial: 10
Full: 9
Yes: 15
No: 4
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Table S2. Details of samples obtained from the Turn Point (WTP) site, San Juan Islands,
Washington. Fire history data are available through the International Multiproxy Paleofire
Database (https://www.ncdc.noaa.gov/paleo/study/26332).
Site Sample
Number
Live? Full or
Partial?
Crossdated? Notes
WTP 2 Yes Partial No 2 pieces
WTP 4 Yes Partial No
WTP 9 No Full Yes No bark
WTP 10 No Full Yes Hollow
WTP 14 Yes Partial Yes
WTP 27 No Full Yes Recorded as live in
field, but cross-dating
indicates otherwise
WTP 28 Yes Partial No 2 pieces
WTP 30 Yes Partial No
WTP 31 Yes Partial No
WTP 36 No Full Yes Rotten
WTP 41 Yes Partial No
WTP 44 Yes Partial No
WTP 47 Yes Partial Yes
WTP 49 No Partial Yes
WTP 52 No Partial Yes 2 pieces
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Site Sample
Number
Live? Full or
Partial?
Crossdated? Notes
WTP 54 Yes Partial No 2 pieces
WTP 57 No Partial Yes
WTP 58 Yes Partial No
WTP 59 Yes Partial No
WTP 60 Yes Partial No 2 pieces; not used
because burned from
inside out
WTP 61 No Full Yes Rotten
WTP Total 21 Yes: 13
No: 8
Partial: 16
Full: 5
Yes: 10
No: 11
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Table S3. Marker years between 1650 and 2011, as identified from increment cores obtained
from 15 Douglas-fir trees at Kellett Bluff. Cores were taken from 16 trees, but core HIM_001
was omitted as crossdating was not completed on it. Plain text indicates narrow markers, and
bold text indicates wide markers. Standardized ring widths are shown in Figure S2. Raw ring
widths are available through the International Tree Ring Databank
(https://www.ncdc.noaa.gov/paleo/study/26250).
1667
1669
1670
1680
1686
1687
1688
1690
1692
1693
1694
1695
1706
1708
1709
1710
1711
1717
1728
1730
1736
1737
1739
1742
1743
1744
1745
1746
1748
1749
1750
1754
1761
1762
1767
1769
1772
1776
1779
1782
1791
1793
1799
1800
1803
1804
1806
1807
1808
1814
1816
1824
1829
1830
1831
1833
1836
1839
1843
1846
1853
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1870
1874
1875
1879
1881
1883
1884
1885
1887
1889
1890
1891
1892
1893
1894
1895
1899
1906
1907
1909
1911
1912
1913
1915
1918
1929
1933
1935
1939
1941
1943
1945
1946
1947
1954
1955
1956
1959
1962
1965
1966
1968
1970
1973
1979
1980
1981
1982
1986
1989
1991
1993
1997
1999
2000
2001
2003
2007
2011
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Table S4. We used Superposed Epoch Analysis to evaluate the degree of climate forcing on fire
regimes. We focused on the 30 years when fire was recorded at 2 or more sites (Figure 5) and
related them to Palmer Drought Severity Index (PDSI) as reconstructed for summer (June-
August). PDSI was obtained from NADA (2018) for the period from 1400-2005. Analysis was
conducted using FHAES (Brewer et al. 2016) and tested the year of the fire and annual lags of up
to 6 years prior to each fire. Confidence intervals (CIs) were generated using 1000 simulations;
all CIs include zero and thus were highly non-significant.
Lag Mean Lower Bound of 95% CI Upper Bound of 95% CI
-6 0.05 -3.94 4.04
-5 0.29 -3.58 4.16
-4 0.01 -3.16 3.17
-3 0.49 -3.74 4.71
-2 0.25 -3.17 3.67
-1 0.68 -3.06 4.42
0 -0.83 -3.96 2.30
Literature Cited
Brewer, P.W., Velásquez, M.E., Sutherland, E.K., and Falk, D.A. 2016. Fire History Analysis
and Exploration System (FHAES). Version 2.0.2 [computer software]. Available from
http://www.fhaes.org. [accessed 29 November 2018]
North American Drought Atlas [NADA]. 2018. Available from
http://drought.memphis.edu/NADA/ [accessed 15 November 2018]
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