Climate variability reflected by tree-ring width and δ 18 O in a heavily glaciated area of the Patagonian Andes since the Little Ice Age
Wolfgang Jens-Henrik Meier(University of Salzburg), Jussi Grießinger(Friedrich-Alexander-Universität Erlangen-Nürnberg), Jakob Wernicke(ThüringenForst), Ricardo Jaña(Instituto Antártico Chileno), Juan Carlos Aravena(Centro de Estudios Científicos), Mihály Braun(HUN-REN Institute for Nuclear Research)
AGU Fall Meeting Abstracts
December 1, 2016
Cited by 0
Related Papers
Long-term decrease in Asian monsoon rainfall and abrupt climate change events over the past 6,700 years
|Proceedings of the National Academy of Sciences|2021|233
Tree rings reveal globally coherent signature of cosmogenic radiocarbon events in 774 and 993 CE
|Nature Communications|2018|177
The influence of decision-making in tree ring-based climate reconstructions
|Nature Communications|2021|166
Elevation and Mass Changes of the Southern Patagonia Icefield Derived from TanDEM-X and SRTM Data
|Remote Sensing|2018|121
An Updated Multi-Temporal Glacier Inventory for the Patagonian Andes With Changes Between the Little Ice Age and 2016
|Frontiers in Earth Science|2018|110