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Examples
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The discrepancy between the HS-shaped Graybill series and the very different appearing Woodhouse, Kienast and Schweingruber series is worrying, although the Hansen-Bristow series has points in common with Graybill.
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The discrepancy between the HS-shaped Graybill series and the very different appearing Woodhouse, Kienast and Schweingruber series is worrying, although the Hansen-Bristow series has points in common with Graybill.
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Kienast, F. and R. J. Luxmoore, 1988. tree ring analysis and conifer growth responses to increased CO2 levels.
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Graumlich 1991 distinguished the two studies on the basis of altitude, but I pointed out that, at Niwot Ridge, the Graybill PIFL site was actually lower in altitude than the Kienast and Luxmoore sites both PCEN.
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Kienast and Luxmoore [1988] was one of the first responses to the Lamarche et al [1984] hypothesis of increased ring width due to CO2 fertilization.
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So an obvious back-tracking question is: did Graybill collect any Engelman spruce and how do they compare with Kienast/Schweingruber?
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Among the Kienast and Luxmoore sites said not to show enhanced growth are two high Colorado Engelman spruce sites Arapahoe at 3400 m; Niwot Ridge at 3320 m.
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One line of criticism on the dendro front, starting with Kienast and Luxmoore 1988, was that they were simply unable to replicate anomalous late 20th century growth in high-altitude conifer chronologies.
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Graumlich 1991 is a criticism of Lamarche et al [1984] and Graybill [1987] from the Kienast and Luxmoore angle.
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Like Kienast and Luxmoore, Schweingruber et al. also concluded that there was little evidence of anomalous growth.
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