What is it about?
The Tibetan Plateau (TP), “Third Pole”, plays an important role in the Asian Monsoon system and atmospheric circulation of the Northern Hemisphere. We developed two temperature reconstructions in eastern TP based on the tree-ring proxies, and compared with CMIP5 climate model simulations. Our results highlight the MCA-LIA transition (ca. 1587 CE) happened about 150 years later in our TP, and earlier onset of industrial-era warming, and linkage between TP temperature and the Atlantic Multi-decadal Oscillation (AMO) at long-term scale. Please see @ https://rdcu.be/bCYS2
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This page is a summary of: Century-scale temperature variability and onset of industrial-era warming in the Eastern Tibetan Plateau, Climate Dynamics, May 2019, Springer Science + Business Media,
DOI: 10.1007/s00382-019-04807-z.
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