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过去千年东亚与全球百年尺度温度同步性变化的模拟研究

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利用美国国家大气研究中心(NCAR)提供的过去千年(850~2005年)集合模拟试验(CESM-LME)资料,在与重建资料、现代观测/再分析资料进行对比验证的基础上,分析了过去千年不同世纪东亚与全球地表温度变化的同步性,并结合单因子敏感性试验结果,分析了造成东亚与全球地表温度各个世纪同步性及变化幅度差异的原因.结果表明:过去千年里,在20世纪以前,东亚地区与全球均经历了中世纪暖期与小冰期,温度变化在百年尺度上整体一致,10世纪、11世纪、13世纪、18世纪和19世纪东亚与全球温度变化同步性较高,差异较小;但在12世纪、14~17世纪中,其变化振幅存在显著差异,东亚地区温度变化幅度总体上小于全球,太阳辐射和火山活动等自然外强迫及内部变率对差异的形成可能起到了主导作用;而20世纪以来,两者变化显示出较大的不同步性,东亚地区温度增长没有全球温度增长剧烈,甚至出现了降温,人为外强迫在这一时期起主导作用.温室气体浓度变化对温度的影响在两极有明显的放大效应,是东亚与全球温度变化差异形成的主要原因,同时,人为气溶胶排放使得东亚地区温度降低也是东亚与全球温度变化不同步的原因之一.
SIMULATION STUDY OF CENTENNIAL SCALE SURFACE TEMPERATURE SYNCHRONICITY CHANGES BETWEEN EAST ASIA AND THE WHOLE WORLD IN THE LAST MILLENNIUM
Changes in surface temperature have a huge impact on the Earth's natural environment and biological systems.Understanding regional temperature variation has become the key to global climate change research.However,there is still a great deal of uncertainty about whether regional surface temperature evolution is consistent with global evolution.The study of the synchronization between East Asia(4°~53°N,105°~140° E)and global centennial scale surface temperature changes in the last millennium can supplement the study of regional surface temperature responses to global changes.In this study,the synchronization and amplitude differences of East Asian and global surface temperature changes in different centuries were studied using the transient simulation experiment(CESM-LME)over the last millennium(850~2005 A.D.).The reasons for the difference between East Asian and global land surface temperature synchronous changes in several centuries are analyzed.This paper draws the following main conclusions.Before the 20th century,East Asia and the world experienced the Medieval Warm Period(MWP)and the Little Ice Age(LIA)for thousands of years.On the centennial scale,the surface temperature fluctuation is generally consistent.In the 10th,11th,13th,18th and 19th centuries,surface temperature fluctuations in East Asia were highly synchronized with those on a global scale,with the smallest differences.In the 12th and 14th to 17th centuries,there was a marked difference in their changes.In the 12th century,the East Asian surface temperature anomaly was 0.047 ℃ lower than the global average.During the 14th to 17th centuries,East Asian temperature anomalies were 0.036 ℃,0.040 ℃,0.032 ℃ and 0.071 ℃ higher than the global average,respectively.The range of temperature change in East Asia is generally smaller than that of the whole world,and natural external forces such as solar radiation,volcanic activity and internal variability play a leading role in the formation of differences.Since the 20th century,however,the two changes have shown a greater divergence,with the East Asian temperature anomaly 0.179 ℃ lower than the global average.In East Asia,land surface temperature has not increased as much as global temperature,or even cooled.Artificial extrinsic forcing has played a dominant role in this period.The effect of greenhouse gas concentration change on polar temperature has a significant amplification effect,which is the main reason for the difference between East Asia and the global temperature change.The cooling caused by anthropogenic aerosol emissions in East Asia is also one of the reasons why East Asia is out of synchronization with global temperature changes.

surface temperature changelast millenniumsimulation studyglobalEast Asiasynchronization

刘雅雯、严蜜、刘健、宁亮

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南京师范大学虚拟地理环境教育部重点试验室/江苏省地理环境演化国家重点试验室培育建设点/江苏省地理信息资源开发与利用协同创新中心,南京师范大学地理科学学院,江苏南京 210023

崂山实验室,山东青岛 266061

江苏省大规模复杂系统数值模拟重点试验室,南京师范大学数学科学学院,江苏南京 210023

温度变化 过去千年 模拟研究 全球 东亚地区 同步性

国家自然科学基金项目国家自然科学基金项目国家自然科学基金项目国家自然科学基金项目国家自然科学基金项目国家自然科学基金国际(地区)合作与交流项目中国科学院地球环境研究所黄土与第四纪地质国家重点实验室开放基金项目中国科学院地球环境研究所黄土与第四纪地质国家重点实验室开放基金项目江苏省高校优势学科建设项目江苏省研究生科研与实践创新计划项目

421306044207504941971108419710214220505542111530182SKLLQG1930SKLLQG1820164320H116KYCX22_1582

2024

第四纪研究
中国科学院地质与地球物理研究所 中国第四纪研究委员会

第四纪研究

CSTPCD北大核心
影响因子:2.939
ISSN:1001-7410
年,卷(期):2024.44(2)
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