地球科学进展 >
2016 , Vol. 31 >Issue 6: 634 - 642
DOI: https://doi.org/10.11867/j.issn.1001-8166.2016.06.0634.
基于树轮资料初探过去千年强火山喷发与青藏高原东部温度变化关系
作者简介:李明启(1979-),男,山东东明人,助理研究员,主要从事树轮气候学研究.E-mail:limq@igsnrr.ac.cn
收稿日期: 2016-03-08
修回日期: 2016-05-20
网络出版日期: 2016-06-10
基金资助
*国家自然科学基金重点项目“过去千年自然外强迫异常期的中国气候变化空间型及其形成机制”(编号:41430528);国家自然科学基金面上项目“横断山区树轮揭示的过去500年火山喷发信号及其气候效应”(编号:41571194)资助
版权
Study on the Relationship between Large Volcanic Eruptions and Temperature Variation Based on Tree-Ring Data in the Eastern Tibetan Plateau during the Past Millennium
First author:Li Mingqi(1979-), male, Dongming County, Shandong Province, Research Assistant. Research areas include the dendroclimatology.E-mail:limq@igsnrr.ac.cn
Received date: 2016-03-08
Revised date: 2016-05-20
Online published: 2016-06-10
Supported by
Project supported by the Key Program of National Natural Science Foundation of China “Spatial patterns of climate change in China driven by the anomalies of natural external forcings during the past millennium”(No.41430528);The General Program of National Natural Science Foundation of China “Volcanic eruption signals from tree-ring and its effect on climate in the Hengduan Mountain area in the past 500 years”(No.41571194)
Copyright
强火山喷发是影响年际至年代际全球气候变化的重要因素之一。基于树木年轮资料重建的6条温度序列,集成重建了青藏高原东北部过去1 300多年和青藏高原东南部过去600多年的温度序列。在过去1 300多年,青藏高原东北部存在3个明显的冷期:670—920年、1000—1310年和1590—1930年;3个明显的暖期:920—1000年、1310—1590年和1930—2000年。青藏高原东南部过去600多年存在2个明显的冷期:1385—1450年和1570—1820年,2个明显的暖期:1450—1570年和1820—2000年。结合火山活动序列年表,利用时序叠加法,初步分析了过去千年强火山喷发对青藏高原东部温度变化的影响。结果表明:10°S~10°N的强火山喷发后第一年青藏高原东部出现降温,并且在α=0.05置信水平上东北部地区降温显著,东南部地区第二年达到降温显著水平;其他纬度的强火山喷发对青藏高原东北部和东南部的温度影响存在一定差异,第一年后两区均发生降温,但均未达到显著水平,然而青藏高原东北部地区第四年降温达到显著水平。这可能主要是由区域差异、不同季节温度对火山活动响应差异,或者火山喷发性质、季节、纬度以及区域的气候背景存在差异引起的。
李明启 , 邵雪梅 . 基于树轮资料初探过去千年强火山喷发与青藏高原东部温度变化关系[J]. 地球科学进展, 2016 , 31(6) : 634 -642 . DOI: 10.11867/j.issn.1001-8166.2016.06.0634.
Volcanic eruptions can significantly cool the global troposphere on the time scales from several months up to a decade due to reflection of solar radiation by sulfate aerosols and feedback mechanisms in the climate system. The impact of volcanic eruptions on global climate are discussed in many studies. However, few studies have been done on the impact of volcanic eruption on climate change in China in the past millennium. The 1300-year and 600-year temperature series were reconstructed based on the six tree-ring temperature proxy data in northeastern and southeastern Tibetan Plateau, respectively. Three warm periods occurred in 670-920,1000-1310 and 1590-1930, and three cold periods happened at 920-1000,1310-1590 and 1930-2000 in the northeastern Tibetan Plateau. There were two obviously warm periods (1385-1450 and 1570-1820) and two cold periods (1450-1570 and 1820-2000) in southeastern Tibetan Plateau. Contrasting with volcanic eruption chronology, we analyzed the relationship between volcanic activity and temperature variation in the eastern Tibetan plateau during the past millennium using Superposed Epoch Analysis (SEA) method. The results indicated that the temperature decreased one year after large volcanic eruptions located beteen 10°S and 10°N in latitude in northeastern Tibetan Plateau and two years in southeastern Tibetan Plateau. The volcanic eruptions occurred at different latitudes have different impacts on the temperature variations, which may be caused by regional difference, the nature of the eruption, the magnitude of the resulting change in incoming solar radiation, prevailing background climate and internal variability, season, latitude, and other considerations.
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