Abstract: Climate variability reflected by tree-ring width and δ<sup>18</sup>O in a heavily glaciated area of the Patagonian Andes since the Little Ice Age (2016 AGU Fall Meeting)

Climate variability reflected by tree-ring width and δ¹⁸O in a heavily glaciated area of the Patagonian Andes since the Little Ice Age

Wolfgang Jens-Henrik Meier¹, Jakob Wernicke Jr.¹, Mathias Braun¹, Juan C Aravena², Ricardo JaÃ±a³ and Jussi Griessinger¹, (1)University of Erlangen-Nuremberg, Erlangen, Germany, (2)Universidad de Magallanes, Gaia Antártica, Punta Arenas, Chile, (3)Instituto Antártico Chileno, Punta Arenas, Chile

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Climate variability reflected by tree-ring width and δ18O in a heavily glaciated area of the Patagonian Andes since the Little Ice Age

Climate variability reflected by tree-ring width and δ¹⁸O in a heavily glaciated area of the Patagonian Andes since the Little Ice Age