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Climate-change impact on the 20th-century relationship between the Southern Annular Mode and global mean temperature

机译:气候变化对20世纪南环空模式与全球平均温度之间关系的影响

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The positive phase of the El Ni?o-Southern Oscillation (ENSO) increases global mean temperature, and contributes to a negative phase of the Southern Annular Mode (SAM), the dominant mode of climate variability in the Southern Hemisphere. This interannual relationship of a high global mean temperature associated with a negative SAM, however, is opposite to the relationship between their trends under greenhouse warming. We show that over much of the 20th century this relationship undergoes multidecadal fluctuations depending on the intensity of ENSO. During the period 1925–1955, subdued ENSO activities weakened the relationship. However, a similar weakening has occurred since the late 1970s despite the strong ENSO. We demonstrate that this recent weakening is induced by climate change in the Southern Hemisphere. Our result highlights a rare situation in which climate change signals emerge against an opposing property of interannual variability, underscoring the robustness of the recent climate change.
机译:厄尔尼诺-南方涛动(ENSO)的正相增加了全球平均温度,并导致南半球模式(SAM)的负相,这是南半球气候变化的主要模式。然而,这种高全球平均温度与负SAM相关的年际关系与温室效应下它们的趋势之间的关系相反。我们表明,在20世纪的大部分时间里,这种关系经历了数十年的波动,具体取决于ENSO的强度。在1925年至1955年期间,ENSO活动的减弱削弱了这种关系。然而,尽管ENSO表现强劲,但自1970年代末以来也发生了类似的减弱。我们证明,最近的这种减弱是由南半球的气候变化引起的。我们的结果突出表明了一种罕见的情况,其中气候变化信号与年际可变性的对立属性相对应,突显了近期气候变化的稳健性。

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