Titlebook: Dendroclimatology; Progress and Prospec Malcolm K. Hughes,Thomas W. Swetnam,Henry F. Diaz Book 2011 Springer Science+Business Media B.V. 20

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https://doi.org/10.1007/978-3-030-39536-0oaches been applied to evaluate regional and broader-scale processes. As with dendroclimatic data (e.g., ring-width and ring-density chronologies), climatic drivers become much more evident in dendroecological data aggregated at broad spatial scales (relative to local-scale data). Study of dendroeco

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How Well Understood Are the Processes that Create Dendroclimatic Records? A Mechanistic Model of thel environmental conditions. The model, here termed Vaganov–Shashkin (VS), reproduces the critical features linking climate variability to tree-ring proxy formation. We discuss recent test simulations of tree-ring width data from a variety of sites and spatiotemporal scales. Our experiments demonstra

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Stable Isotopes in Dendroclimatology: Moving Beyond ‘Potential’hree elements carry signals that can be interpreted in terms of past climate because isotope ratios are climatically controlled by the tree’s water and gas exchange budgets. The traditional tree-ring proxies form the most widespread and arguably the most valuable of the high-resolution climate archi