2016
DOI: 10.1007/s00382-016-3465-0
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Decadal modulation of the ENSO–East Asian winter monsoon relationship by the Atlantic Multidecadal Oscillation

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Cited by 58 publications
(50 citation statements)
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References 76 publications
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“…This AMO phase dependence of the La Niña‐EAWM connection (Figure b) is consistent with the AMO phase dependence in the correlation between Niño3.4 index and the EAWMI (Figure c). These results are consistent with our recent study proposing a nonlinear decadal modulation of the ENSO‐EAWM relationship by the AMO (Geng et al, ). These observational results suggest that the AMO seems to play an important role in the nonstationarity of the ENSO‐EAWM relationship.…”
Section: Application To the Nonstationary Enso‐eawm Relationshipsupporting
confidence: 94%
See 1 more Smart Citation
“…This AMO phase dependence of the La Niña‐EAWM connection (Figure b) is consistent with the AMO phase dependence in the correlation between Niño3.4 index and the EAWMI (Figure c). These results are consistent with our recent study proposing a nonlinear decadal modulation of the ENSO‐EAWM relationship by the AMO (Geng et al, ). These observational results suggest that the AMO seems to play an important role in the nonstationarity of the ENSO‐EAWM relationship.…”
Section: Application To the Nonstationary Enso‐eawm Relationshipsupporting
confidence: 94%
“…Recent observational analyses, however, suggest that this ENSO‐EAWM relationship seems to vary over time and exhibits pronounced multidecadal fluctuations (e.g., He & Wang, ; Zhou et al, ). The waxing and waning of the statistical ENSO‐EAWM relationship is usually explored based on running correlation analysis and is argued to be associated with changes in slow background forcings, ranging from the modulation effect by solar activity (Zhou et al, ), the Pacific Decadal Oscillation (PDO) (Wang et al, ), the Atlantic Multidecadal Oscillation (AMO) (Geng et al, ), and both the PDO and AMO (He & Wang, ; Kim et al, ). At present, the causes of the decadal variation, or apparent nonstationarity, of the ENSO‐EAWM relationship remain a subject of active debate.…”
Section: Introductionmentioning
confidence: 99%
“…Wang and He () had pointed out that the EAWM–ENSO relationship is weakened in the mid‐1970s and this weakening was induced by the decadal weakening of the EAWM and the inter‐decadal variations of SST anomalies related to ENSO. The Pacific Decadal Oscillation (PDO) and Atlantic Multi‐decadal Oscillation (AMO) have modulation effects on the variations of atmosphere and their relationship with ENSO (Wang et al, ; Yoon and Yeh, ; He and Wang, ; Geng et al, ; Kim et al, ). During the positive phase of PDO (or negative phase of AMO), the correlation between EAWM and ENSO is not robust.…”
Section: Introductionmentioning
confidence: 99%
“…During the positive phase of PDO (or negative phase of AMO), the correlation between EAWM and ENSO is not robust. During the negative phase of PDO (or positive phase of AMO), ENSO could exert strong impacts on the EAWM (Wang et al, ; Geng et al, ; Kim et al, ). Moreover, Kim et al .…”
Section: Introductionmentioning
confidence: 99%
“…These climate changes range from decadal to centennial and millennial variations, and have been well documented through historical and proxy records, particularly annual growth rings in trees, cave stalagmites, corals, cores of lake and deep-sea sediments and ice cores (Mc-Manus et al, 1994;Jones et al, 2009;Esper et al, 2002). Interannual and decadal climate oscillations include El Niño-Southern Oscillation, the North Atlantic Oscillation, the Pacific Decadal Oscillation or the Atlantic Multidecadal Oscillation (Henley et al, 2015;Geng et al, 2017;Kayano et al, 2019). They have also been associated to the collapse of the Maya civilization in Mesoamerica between the 8th and 9th centuries, suggesting that intense droughts may have led to social stresses (Hodell et al, 1995;Haug et al, 2003;Douglas et al, 2015;Beach et al, 2016).…”
mentioning
confidence: 99%