Centennial-Scale Variability in Atmospheric Circulation in Antarctica: Insights From a Coastal East Antarctic Ice Core Record

IF 3.8 2区 地球科学 Q2 METEOROLOGY & ATMOSPHERIC SCIENCES
Zhe Li, Guitao Shi, Su Jiang, Danhe Wang, Bo Zhang, Tianming Ma, Jinhai Yu, Jingxue Guo
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Abstract

A 108-m ice core (32SC) spanning the period from 1616 to 2016 CE was retrieved from coastal Princess Elizabeth Land (PEL), East Antarctica (69.97°S, 76.52°E, 1,113 m elevation). The ice core was analyzed to investigate the relationship between sea salt aerosols (SSAs), sea ice dynamics, and atmospheric circulation. The first component of Empirical Orthogonal Function analysis (32SC REOF1), which explains 58% of the variance in the ice core ions, serves as a proxy for SSAs. Time series correlation analysis reveals that sea ice had a minimal impact on 32SC REOF1. Instead, it showed a significant correlation with winter meridional atmospheric transport from the Southern Indian Ocean to PEL. The sea salt records exhibit a significant increase from the period 1616–1850 to 1851–2016 CE, with the mean value increasing by a factor of 2.4. This centennial-scale trend is likely linked to shifts in the position of the Southern Hemisphere Westerly Winds (SHWW). During the earlier period (1616–1850 CE), which was likely characterized by a colder climate, the SHWW in the Southern Indian Ocean sector may have shifted equatorward and weakened in intensity, potentially leading to reduced cyclone frequency and a subsequent decline in SSAs transport to high latitudes. In contrast, the period 1851–2016 CE, which is likely warmer, saw the SHWW shifted poleward, enhancing meridional wind speeds and increasing SSAs transport. Comparisons with other Antarctic ice core records suggest that the centennial-scale shift in the SHWW is a regional phenomenon, particularly pronounced in the Southern Indian Ocean.

南极大气环流的百年尺度变率:来自南极东部沿海冰芯记录的见解
从东南极洲沿海伊丽莎白公主地(69.97°S, 76.52°E,海拔1113 m)获取了1616 - 2016 CE期间的108 m冰芯(32SC)。通过对冰芯的分析,探讨了海盐气溶胶、海冰动力学和大气环流之间的关系。经验正交函数分析(32SC REOF1)的第一分量解释了冰芯离子中58%的方差,可以作为SSAs的代理。时间序列相关分析表明,海冰对32SC REOF1的影响最小。相反,它与冬季从南印度洋到PEL的经向大气输送有显著的相关性。海盐记录在1616-1850年至1851-2016年期间呈显著上升趋势,平均上升了2.4倍。这种百年尺度的趋势可能与南半球西风(SHWW)位置的变化有关。在早期(公元1616-1850年),南印度洋区域的西南副热带可能向赤道方向移动,强度减弱,可能导致气旋频率减少,随后南印度洋向高纬度地区输送的南印度洋副热带减少。相比之下,1851年至2016年东经时间可能偏暖,西南副热带向极地移动,增强了经向风速,增加了ssa输送。与其他南极冰芯记录的比较表明,西南海温百年尺度的转变是一种区域现象,在南印度洋尤为明显。
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来源期刊
Journal of Geophysical Research: Atmospheres
Journal of Geophysical Research: Atmospheres Earth and Planetary Sciences-Geophysics
CiteScore
7.30
自引率
11.40%
发文量
684
期刊介绍: JGR: Atmospheres publishes articles that advance and improve understanding of atmospheric properties and processes, including the interaction of the atmosphere with other components of the Earth system.
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