树轮数据揭示的强火山喷发对青藏高原地区气候的影响

doi:10.13287/j.1001-9332.202110.009

应用生态学报 ›› 2021, Vol. 32 ›› Issue (10): 3771-3780.doi: 10.13287/j.1001-9332.202110.009

所属专题：树轮生态学专栏

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树轮数据揭示的强火山喷发对青藏高原地区气候的影响

聂文政^1,2, 李明启^1,2*

¹中国科学院地理科学与资源研究所, 中国科学院陆地表层格局与模拟重点实验室, 北京 100101;
²中国科学院大学, 北京 100049

收稿日期:2021-04-08 修回日期:2021-06-30 出版日期:2021-10-15 发布日期:2022-04-15
通讯作者: * E-mail: limq@igsnrr.ac.cn
作者简介:聂文政, 男, 1998年生, 硕士研究生。主要从事树木年轮气候学研究。E-mail: niewenzheng20@mails.ucas.ac.cn
基金资助:
国家重点研发计划项目(2017YFA0603302)和国家自然科学基金项目(41571194,41630529)资助

Influence of large volcanic eruptions on climate as revealed by tree-ring data on the Tibetan Plateau, China

NIE Wen-zheng^1,2, LI Ming-qi^1,2*

¹Key Laboratory of Land Surface Pattern and Simulation, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China;
²University of Chinese Academy of Sciences, Beijing 100049, China

Received:2021-04-08 Revised:2021-06-30 Online:2021-10-15 Published:2022-04-15
Contact: * E-mail: limq@igsnrr.ac.cn
Supported by:
National Key R&D Program of China (2017YFA0603302) and the National Natural Science Foundation of China (41571194, 41630529).

摘要/Abstract

摘要： 强火山喷发是影响全球气候变化的重要因素。过去几十年,不同学者基于青藏高原地区树木年轮重建了多条气候变化序列,并依据这些序列研究了全球强火山喷发对青藏高原地区气候的影响。结果表明: 探讨强火山喷发对青藏高原气候影响的树轮序列主要分布在青藏高原东部。利用序列对比法和时序叠加法分析发现,中低纬度的强火山喷发对青藏高原地区温度和干湿变化影响显著,并在强火山喷发后的1～2年内出现降温或者发生干旱,而高纬度的强火山喷发影响较小。此外,连续的多次强火山喷发能导致该区出现年代际的冷期。影响强火山喷发气候效应的因素主要包括火山喷发位置、喷发强度、大气环流等。最后结合国内外研究现状,对未来需要开展的研究方向进行了展望。

关键词: 树轮数据, 强火山喷发, 青藏高原, 温度, 干湿变化

Abstract: Large volcanic eruption is an important factor affecting global climate change. In the past few decades, many researchers reconstructed a number of climate series based on tree rings on the Tibetan Plateau, and examined the impacts of large volcanic eruptions on the climate. The results showed that these tree-ring sites used to examined the influences of large volcanic eruptions on climate change were primarily located in the eastern Tibetan Plateau. In addition, the series comparison and the superposed epoch analysis were main methods for studying the climate effects of large volcanic eruptions. Based on the results analyzed using two methods, we suggested that the large volcanic eruptions in low-mid latitudes had a significant impact on temperature and dry/wet variation. Cooling or drought occurred after large volcanic eruptions in the subsequent 1-2 years. How-ever, the large volcanic eruptions in high latitudes had minor impacts on climate change. Furthermore, consecutive multiple volcanic eruptions could result in cooling at the decades scale. The factors influencing the climate effects of large volcanic eruptions included the location of the volcanic eruptions, intensity of the volcanic eruptions, atmospheric circulation, etc. Finally, we proposed research projects that need to be carried out in the future.

Key words: tree-ring data, large volcanic eruption, Tibetan Plateau, temperature, dry/wet variation

聂文政, 李明启. 树轮数据揭示的强火山喷发对青藏高原地区气候的影响[J]. 应用生态学报, 2021, 32(10): 3771-3780.

NIE Wen-zheng, LI Ming-qi. Influence of large volcanic eruptions on climate as revealed by tree-ring data on the Tibetan Plateau, China[J]. Chinese Journal of Applied Ecology, 2021, 32(10): 3771-3780.

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树轮数据揭示的强火山喷发对青藏高原地区气候的影响

Influence of large volcanic eruptions on climate as revealed by tree-ring data on the Tibetan Plateau, China

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