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首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >Short Communication The strengthening relationship between Arctic Oscillation and ENSO after the mid-1990s
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Short Communication The strengthening relationship between Arctic Oscillation and ENSO after the mid-1990s

机译:短期交流1990年代中期以后,北极涛动与ENSO之间的关系加强

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The Arctic Oscillation (AO) and ENSO have dominant influences on the extratropical and tropical climate variabilities in the Northern Hemisphere, respectively. In this paper, we document a strengthening of the AO-ENSO relationship in January after the mid-1990s, when the interannual variability of the previous September Arctic sea ice cover (ASIC) had consistently increased, by analyzing the AO, ENSO, and associated atmosphere-ocean variability. Our analysis further suggests that the larger ASIC interannual variability may account for the larger scale wave train across the Pacific basin, and the AO is strongly coupled to the circulation in the North Pacific. The strengthened connection between the ?AO and Aleutian Low (AL) may contribute to the identified closer relationship between the ?AO and ENSO.
机译:北极涛动(AO)和ENSO分别对北半球的温带和热带气候变异有主要影响。在本文中,我们通过分析AO,ENSO及其相关因素,证明了1990年代中期之后1月份AO-ENSO关系的加强,当时前9月的北极海冰盖(ASIC)的年际变化一直在增加。大气-海洋变化。我们的分析进一步表明,较大的ASIC年际变化可能解释了整个太平洋海盆的较大规模的波列,并且AO与北太平洋的环流强烈相关。 ?AO和阿留申低点(AL)之间的加强联系可能有助于确定?AO和ENSO之间的更紧密关系。

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