2014
DOI: 10.1175/bams-d-13-00201.1
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Decadal Climate Variability and Cross-Scale Interactions: ICCL 2013 Expert Assessment Workshop

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Cited by 11 publications
(9 citation statements)
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“…ENSO properties vary on decadal and longer time scales (e.g., Holbrook et al 2014;Wittenberg 2015;Power and Smith 2007) through changes in air-sea feedbacks linked to noise, chaotic dynamics, and slow variations in the mean state (e.g., Wittenberg 2009;Newman et al 2011;Wittenberg et al 2014;Zhao et al 2016). While the mean-state variations are thought to be in part a rectified effect of changes in ENSO (e.g., Ogata et al 2013), they also affect the interactions between ENSO and other modes of variability such as the SAM (e.g.…”
Section: Low Frequency Variabilitymentioning
confidence: 99%
“…ENSO properties vary on decadal and longer time scales (e.g., Holbrook et al 2014;Wittenberg 2015;Power and Smith 2007) through changes in air-sea feedbacks linked to noise, chaotic dynamics, and slow variations in the mean state (e.g., Wittenberg 2009;Newman et al 2011;Wittenberg et al 2014;Zhao et al 2016). While the mean-state variations are thought to be in part a rectified effect of changes in ENSO (e.g., Ogata et al 2013), they also affect the interactions between ENSO and other modes of variability such as the SAM (e.g.…”
Section: Low Frequency Variabilitymentioning
confidence: 99%
“…In line with the great volume of the Southern Hemisphere (SH) oceans, the South Pacific Ocean exhibits prominent decadal climate variability (e.g., Reason 2000). That said, our understanding of Pacific and in particular South Pacific decadal variability and predictability has been limited, despite this being an emerging area of substantial interest and active research (Meehl et al 2014;Holbrook et al 2014;Power et al 2017). The lack of consistent long-term observations has in part led to less attention being drawn to the South Pacific.…”
Section: Introductionmentioning
confidence: 99%
“…As with other parts of the globe, internally generated climate variability is a major element of SH MDCV (Kirtman et al, 2013). Major components of internal variability for the Southern Hemisphere are decadal variations in ENSO, the Interdecadal Pacific Oscillation (IPO, Garreaud and Battisti, 1999;Power et al, 1999;Salinger et al, 2001;Folland et al, 2002;Wu and Hsieh, 2003;Holbrook et al, 2011;Christensen et al, 2013;Kosaka and Xie, 2013;England et al, 2014;Holbrook et al, 2014;Watanabe et al, 2014;Henley et al, 2015;, the Southern Annular Mode (SAM (Shiotani, 1990;Thompson et al, 2000;Watterson, 2009;Pohl et al, 2009;Yuan and Yonekura, 2011;Jones et al, 2016), and the Indian Ocean Dipole.…”
Section: Causes Of Sh MDCVmentioning
confidence: 99%