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Asymmetric vegetation responses, variation among and within proxies, and the near-absence of fire today suggest caution in using changes associated with mid-Holocene aridity at the prairie forest boundary as an analog for future responses to global warming.
The noise in the responses (variation between experimental and predicted values) was measured with the lack of fit P values and the values were 3.8 and 5.2% for Y 2 and Y 1 respectively, which were less than observed values (<14.4%) in the literature (Im et al. 2012).
Despite the small number of responses, variation in agreement is clearly evident.
For some responses, variation between sites was not significant; subsequent analyses were then simplified to ordinary nonhierarchical GLMs.
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They, too, have seen ash dieback and here on this street have come up with their response: variation.
An AS is a linear manifold of the stochastic space characterized by maximal response variation.
The parameter pH alone could explain 75.5% of the response variation.
Subsequently, the peak response variation as well as orbit orientation changes have been studied experimentally.
Finally, the correlation-free upper bounds of response variation are proposed for the practical purpose.
Outcome measures used to evaluate the effectiveness of AR cueing included: Time-to-Contact (TTC), Gap Time Variation (GTV), Response Rate, and Gap Response Variation (GRV).
The FIA response was highly reproducible, and the response variation was below 6% from film to film in detectable range.
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