Detection of climate signal in dendrochronological data analysis: a comparison of tree-ring standardization methods

By S. Helama, M. Lindholm, M. Timonen, M. Eronen. 2004

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A new stochastic model of episode peak and duration for eco-hydro-climatic applications (2008, unknown): “(Biondi, 1993; Cook and Peters, 1997; Biondi, 1999; Helama et al., 2004).”
Bioclimatology of beech (Fagus sylvatica L.) in the Eastern Alps: spatial and altitudinal climatic signals identified through a tree‐ring network (2007, background): “Although ‘standardized indices’ used in dendrochronology are often calculated as ratios between the measurement and the fitted curve value, there is evidence that variance-stabilized residuals should be preferred (Cook & Peters, 1997; Biondi, 1999; Helama et al., 2004).”
Revisiting long-range dependence in annual precipitation (2018, methodology): “This methodology has a severe impact on the low-frequency 245 variability [Briffa et al., 1996; Helama et al., 2004], and thus on H estimation, as presented in 246 Figure 2 (red diagonal lines).”