地球科学进展 ›› 2021, Vol. 36 ›› Issue (2): 172 -184. doi: 10.11867/j.issn.1001-8166.2021.012

研究论文 上一篇    下一篇

东南极 LGB69冰芯 17122001年气温变化记录的初步研究
张子洋 1 , 2( ), 闫明 1( ), MULVANEY Robert 3, 季峻峰 2, 效存德 4, 刘雷保 1, 安春雷 1   
  1. 1.中国极地研究中心,上海 200136
    2.南京大学表生地球化学教育部重点实验室,江苏 南京 210023
    3.British Antarctic Survey,High Cross,Madingley Road,Cambridge CB3 0ET,UK
    4.中国科学院 西北生态环境资源研究院,甘肃 兰州 730000
  • 收稿日期:2020-07-25 修回日期:2021-01-05 出版日期:2021-06-25
  • 通讯作者: 闫明 E-mail:zhzyang@139.com;mingyan@pric.org.cn
  • 基金资助:
    国家自然科学基金项目“极地冰芯中记录的火山作用及其对气候的影响”(41676192)

Preliminary Study on Air Temperature Records from 1712 to 2001 Revealed by LGB69 Ice Core in East Antarctica

Ziyang ZHANG 1 , 2( ), Ming YAN 1( ), Robert MULVANEY 3, Junfeng JI 2, Cunde XIAO 4, Leibao LIU 1, Chunlei AN 1   

  1. 1.Polar Research Institute of China,Shanghai 200136,China
    2.Key Laboratory of Surficial Geochemistry,Ministry of Education,Nanjing University,Nanjing 210023,China
    3.British Antarctic Survey,High Cross,Madingley Road,Cambridge CB3 0ET,UK
    4.Northwest Institue of Eco-Environment and Resources,Chinese Academy of Sciences,Lanzhou 730000,China
  • Received:2020-07-25 Revised:2021-01-05 Online:2021-06-25 Published:2021-04-19
  • Contact: Ming YAN E-mail:zhzyang@139.com;mingyan@pric.org.cn
  • About author:ZHANG Ziyang (1991-), male, Zhongshan County, Guangdong Province, Master student. Research areas include polar environmental geochemistry. E-mail: zhzyang@139.com
  • Supported by:
    the National Natural Science Foundation of China "Volcanism recorded in polar ice cores and its effects on climate"(41676192)

南极冰芯记录着过去气温、降水等气候环境参数以及影响其变化的太阳活动、火山作用等各种因子变化,是研究古气候、古环境变化及其影响机制的良好载体。东南极LGB69冰芯高分辨率的地球化学分析表明: 该冰芯的水当量年平均积累率高达259 mm/a,利用δ18O和Na+季节性变化和火山喷发标志层,通过数年层的方法确定其沉积时间为290 a(1712—2001年)±2 a; 该冰芯δ18O与邻近的戴维斯站气温距平5年滑动平均值(1968—2001年)之间具有良好的正相关关系,是有效的气温代用指标,1712—2001年该地区气温是一个波动变暖的过程,划分为4个阶段,小冰期结束于1914年,20世纪5年滑动平均气温距平年平均值较小冰期末次冷阶段升高0.43 ℃; Morlet小波分析表明,1712—2001年该冰芯δ18O(气温)和积累率(降水量)均存在约11年、约22年和约60年的共同周期,多重时间周期的嵌套表明其对气候变化非常敏感。上述研究结果为进一步重建南极气候冷暖、降水序列变化,以及研究太阳活动、火山作用等因子对气候变化影响的内在规律奠定了基础。

Antarctic ice core is an ideal paleoclimatic and paleoenvironmental carrier, which records the past variations of various parameters such as air temperature, precipitation and their major factors, e.g. solar activity, volcanism. High-resolution geochemical analyses of LGB69 ice core, East Antarctica show that Based on the combination of seasonal variations of δ18O and Na+ with volcanic eruption markers, LGB69 ice core is dated to 290 a (A.D.1712-A.D.2001)±2 a through annual layer counting, with a high average annual accumulation rate of 259 mm w.e./a; Five-year moving average (A.D.1968-A.D.2001) of δ18O of LGB69 ice core has good positive correlation with that of temperature departure at adjacent Davis Station, indicating that δ18O is an effective proxy for air temperature. Air temperature from A.D.1712 to A.D.2001 in LGB69 region is a process of fluctuating warming, which can be divided into four stages. The average annual value of 5-year moving average temperature departure is 0.43 ℃ higher than that of last cold stage in the Little Ice Age which ended in A.D.1914; By Morlet wavelet analysis, both δ18O (air temperature) and accumulation rate (precipitation) of LGB69 ice core from A.D.1712 to A.D.2001 present ca. 11-year, ca. 22-year and ca. 60-year cycles. Multinest of cycles for δ18O, accumulation rate of LGB69 ice core implies its sensitivity to climate change. The above-mentioned results build up a good basis for further research on the reconstruction of temporal variations in air temperature and precipitation and the effects of factors such as solar activity, volcanism on climate change in Antarctica.

中图分类号: 

图1 东南极LGB69冰芯所在位置
Fig.1 The location of LGB69 ice core at East Antarctica
图1 东南极LGB69冰芯所在位置
Fig.1 The location of LGB69 ice core at East Antarctica
图2 冰芯取样横切面
Fig.2 The cross section of ice core sampling
图2 冰芯取样横切面
Fig.2 The cross section of ice core sampling
图3 LGB69冰芯野外实测密度与深度散点图
Fig.3 The scatter diagram of density versus depth of LGB69 ice core
图3 LGB69冰芯野外实测密度与深度散点图
Fig.3 The scatter diagram of density versus depth of LGB69 ice core
图4 LGB69冰芯nssSO 4 2 - 浓度记录的火山喷发信号
Fig.4 Volcanic eruption signals recorded by the nssSO 4 2 - concentrations of LGB69 ice core
图4 LGB69冰芯nssSO 4 2 - 浓度记录的火山喷发信号
Fig.4 Volcanic eruption signals recorded by the nssSO 4 2 - concentrations of LGB69 ice core
表1 LGB69冰芯中火山喷发信号记录
Table 1 Volcanic eruption signal recorded by LGB69 ice core
表1 LGB69冰芯中火山喷发信号记录
Table 1 Volcanic eruption signal recorded by LGB69 ice core
图5 LGB69冰芯δ18ONa+nssSO 4 2 - 变化序列和定年结果
Fig.5 The temporal variations of δ18ONa+nssSO 4 2 - and the dating result of LGB69 ice core
图5 LGB69冰芯δ18ONa+nssSO 4 2 - 变化序列和定年结果
Fig.5 The temporal variations of δ18ONa+nssSO 4 2 - and the dating result of LGB69 ice core
图6 19582001LGB69冰芯δ18O和戴维斯站气温距平5年滑动平均曲线
Fig.6 The 5-year moving average of δ18O of LGB69 ice core and temperature departure of Davis Station from 1958 to 2001
图6 19582001LGB69冰芯δ18O和戴维斯站气温距平5年滑动平均曲线
Fig.6 The 5-year moving average of δ18O of LGB69 ice core and temperature departure of Davis Station from 1958 to 2001
图7 19682001LGB69冰芯δ18O与戴维斯站气温距平5年滑动平均散点图
Fig.7 The 5-year moving average scatter diagram of δ18O of LGB69 ice core and temperature departure of Davis Station from 1968 to 2001
图7 19682001LGB69冰芯δ18O与戴维斯站气温距平5年滑动平均散点图
Fig.7 The 5-year moving average scatter diagram of δ18O of LGB69 ice core and temperature departure of Davis Station from 1968 to 2001
图8 17122001LGB69冰芯δ18O和气温距平5年滑动平均曲线
Fig.8 The 5-year moving average of δ18O and temperature departure of LGB69 ice core from 1712 to 2001
图8 17122001LGB69冰芯δ18O和气温距平5年滑动平均曲线
Fig.8 The 5-year moving average of δ18O and temperature departure of LGB69 ice core from 1712 to 2001
表2 LGB69冰芯不同阶段 5年滑动平均 δ18O年平均值和气温距平年平均值
Table 2 The average annual values of 5-year moving average of δ 18O and temperature departure in different stages of LGB69 ice core
表2 LGB69冰芯不同阶段 5年滑动平均 δ18O年平均值和气温距平年平均值
Table 2 The average annual values of 5-year moving average of δ 18O and temperature departure in different stages of LGB69 ice core
图9 17122001LGB69冰芯δ18O距平小波方差(a)和Morlet小波变换(b
Fig.9 The wavelet variance a and Morlet wavelet transform b of δ18O departure of LGB69 ice core from 1712 to 2001
图9 17122001LGB69冰芯δ18O距平小波方差(a)和Morlet小波变换(b
Fig.9 The wavelet variance a and Morlet wavelet transform b of δ18O departure of LGB69 ice core from 1712 to 2001
图10 17122001LGB69冰芯积累率距平小波方差(a)和Morlet小波变换(b
Fig.10 The wavelet variance a and Morlet wavelet transform b of accumulation rate departure of LGB69 ice core from 1712 to 2001
图10 17122001LGB69冰芯积累率距平小波方差(a)和Morlet小波变换(b
Fig.10 The wavelet variance a and Morlet wavelet transform b of accumulation rate departure of LGB69 ice core from 1712 to 2001
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