Abstract. We evaluate a range of blue intensity (BI) tree-ring
parameters in eight conifer species (12 sites) from Tasmania and New Zealand
for their dendroclimatic potential, and as surrogate wood anatomical
proxies. Using a dataset of ca. 10–15 trees per site, we measured earlywood
maximum blue intensity (EWB), latewood minimum blue intensity (LWB), and the
associated delta blue intensity (DB) parameter for dendrochronological
analysis. No resin extraction was performed, impacting low-frequency trends.
Therefore, we focused only on the high-frequency signal by detrending all
tree-ring and climate data using a 20-year cubic smoothing spline. All BI
parameters express low relative variance and weak signal strength compared
to ring width. Correlation analysis and principal component regression
experiments identified a weak and variable climate response for most
ring-width chronologies. However, for most sites, the EWB data, despite weak
signal strength, expressed strong coherence with summer temperatures.
Significant correlations for LWB were also noted, but the sign of the
relationship for most species is opposite to that reported for all conifer
species in the Northern Hemisphere. DB results were mixed but performed
better for the Tasmanian sites when combined through principal component
regression methods than for New Zealand. Using the full
multi-species/parameter network, excellent summer temperature calibration
was identified for both Tasmania and New Zealand ranging from 52 % to
78 % explained variance for split periods (1901–1950/1951–1995), with
equally robust independent validation (coefficient of efficiency = 0.41 to
0.77). Comparison of the Tasmanian BI reconstruction with a quantitative
wood anatomical (QWA) reconstruction shows that these parameters record
essentially the same strong high-frequency summer temperature signal.
Despite these excellent results, a substantial challenge exists with the
capture of potential secular-scale climate trends. Although DB, band-pass,
and other signal processing methods may help with this issue, substantially
more experimentation is needed in conjunction with comparative analysis with
ring density and QWA measurements.