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- W4239761107 abstract "Abstract. Volcanic eruptions have a significant impact on global temperature; their consequences are of particular interest in regions that are especially sensitive to climate change, like the Tibetan Plateau. In this study, we develop a temperature-sensitive tree-ring width standard chronology covering the period 1348–2014 AD using Qilian juniper (Sabina przewalskii Kom.) samples collected from Animaqin Mountain on the Tibetan Plateau. We reconstruct the annual (prior August to current July) mean minimum temperature (Tmin) since 1380 AD and show that our reconstruction explains 58 % of the variance during the 1960–2014 calibration period. Our results demonstrate in 77.8 % of cases in which a volcanic eruption with a volcanic explosivity index of 5 or greater occurs, temperature decreases in the year of or the year following the eruption. The results of the Superposed Epoch Analysis also indicate that there is a high probability that the Tmin decreases within 2 years of a large volcanic eruption, especially when such eruptions occur in low latitudes." @default.
- W4239761107 created "2022-05-12" @default.
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- W4239761107 date "2020-08-10" @default.
- W4239761107 modified "2023-10-03" @default.
- W4239761107 title "The response of annual minimum temperature on the eastern central Tibetan Plateau to large volcanic eruptions for the period 1380–2014 AD" @default.
- W4239761107 doi "https://doi.org/10.5194/cp-2020-93" @default.
- W4239761107 hasPublicationYear "2020" @default.
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