Key Laboratory of Land Surface Pattern and Simulation, Institute of
Geographic Sciences and Natural Resources, Chinese Academy of Sciences
(CAS), Beijing, 100101, China
CAS Center for Excellence in Tibetan Plateau Earth Sciences, Chinese Academy of Sciences (CAS), Beijing, 100101, China
Institute of Tibetan Plateau Research, Chinese Academy of Sciences (CAS),
Beijing, 100101, China
Xuemei Shao
Key Laboratory of Land Surface Pattern and Simulation, Institute of
Geographic Sciences and Natural Resources, Chinese Academy of Sciences
(CAS), Beijing, 100101, China
College of Resources and Environment, University of Chinese Academy of Sciences, Beijing, 100049, China
Key Laboratory of Land Surface Pattern and Simulation, Institute of
Geographic Sciences and Natural Resources, Chinese Academy of Sciences
(CAS), Beijing, 100101, China
Mingqi Li
Key Laboratory of Land Surface Pattern and Simulation, Institute of
Geographic Sciences and Natural Resources, Chinese Academy of Sciences
(CAS), Beijing, 100101, China
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Total article views: 2,063 (including HTML, PDF, and XML)
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1,418
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Total article views: 2,528 (including HTML, PDF, and XML)
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Total article views: 2,063 (including HTML, PDF, and XML)
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Total article views: 465 (including HTML, PDF, and XML)
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It is not clear to what extent or in what manner a strong volcanic eruption will influence temperature in different regions over the long term. Therefore, new 635-year annual mean minimum temperatures (Tmin) across the eastern central Tibetan Plateau were used to explored the response of Tmin to strong volcanic eruptions. Our results show 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.
It is not clear to what extent or in what manner a strong volcanic eruption will influence...