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首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >Variability in the ENSO-induced southern hemispheric circulation and Antarctic sea ice extent
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Variability in the ENSO-induced southern hemispheric circulation and Antarctic sea ice extent

机译:ENSO引起的南半球环流和南极海冰范围的变化

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摘要

The linkages between the El Ni?o Southern Oscillation (ENSO) and the sea ice extent (SIE) in the Weddell Sea (South Atlantic) and the Bellingshausen-Amundsen Sea (South-Eastern Pacific) sectors of the Southern Ocean have been studied for the period 1979-2005 using crosswavelet analysis. The analysis showed that the relationship between the tropical expression of ENSO and the SIE in these two areas are different before and after 1992. Further, we investigated the structure and strength of the regional Ferrel cell (RFC) during El Ni?o and La Ni?a episodes using composite latitude-pressure cross-sections of wind anomalies for these two periods. Contrasting features were observed in the structure and strength of the RFC before and after 1992 in both, the South Atlantic and the South-Eastern Pacific. These modulations in the RFC control the heat transport from the tropics to high latitudes and hence the extent of sea ice in both the regions. We propose that the modulation of the RFC is responsible for the phase shift in the tropical-polar teleconnection.
机译:研究了厄尔尼诺南方涛动(ENSO)与韦德海(南大西洋)和南太平洋贝灵豪森-阿蒙森海(东南太平洋)海冰范围(SIE)之间的联系,使用交叉小波分析的1979-2005年。分析表明,1992年前后这两个地区ENSO和SIE的热带表达之间的关系是不同的。此外,我们研究了El Ni?o和La Ni期间区域Ferrel细胞(RFC)的结构和强度。 ?这两个时段使用风异常的复合纬度-压力横截面的发作。在1992年之前和之后,在南大西洋和东南太平洋,RFC的结构和强度都有明显的不同。 RFC中的这些调制控制着从热带到高纬度的热传输,因此控制了两个地区的海冰范围。我们建议对RFC的调制负责热带极遥连接中的相移。

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