2003
DOI: 10.1175/1520-0442(2003)016<3853:evotpd>2.0.co;2
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ENSO-Forced Variability of the Pacific Decadal Oscillation

Abstract: Variability of the Pacific decadal oscillation (PDO), on both interannual and decadal timescales, is well modeled as the sum of direct forcing by El Niño-Southern Oscillation (ENSO), the ''reemergence'' of North Pacific sea surface temperature anomalies in subsequent winters, and white noise atmospheric forcing. This simple model may be taken as a null hypothesis for the PDO, and may also be relevant for other climate integrators that have been previously related to the PDO.

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Cited by 599 publications
(461 citation statements)
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“…The PDO is defined as the leading empirical orthogonal function (EOF) of sea surface temperature (SST) anomaly over the North Pacific ([20°N), and the leading principal component (PC1) is referred to as the PDO index (e.g., Mantua et al 1997;Minobe 1997;Zhang et al 1997;Garreaud and Battisti 1999; see review papers by Alexander 2010;Liu 2012). It is significantly correlated with ENSO (e.g., Alexander et al 2002;Newman et al 2003;Deser et al 2004;Schneider and Cornuelle 2005;Vimont 2005). On decadal timescales, the PDO is highly correlated with ENSO (Zhang and Church 2012) and the Interdecadal Pacific Oscillation (IPO), a basin-wide decadal climate mode associated with decadal SST variability in the Pacific (e.g., Power et al 1999;Folland et al 2002;Meehl and Hu 2006).…”
Section: Pdo-related Sea Level Patternsmentioning
confidence: 99%
“…The PDO is defined as the leading empirical orthogonal function (EOF) of sea surface temperature (SST) anomaly over the North Pacific ([20°N), and the leading principal component (PC1) is referred to as the PDO index (e.g., Mantua et al 1997;Minobe 1997;Zhang et al 1997;Garreaud and Battisti 1999; see review papers by Alexander 2010;Liu 2012). It is significantly correlated with ENSO (e.g., Alexander et al 2002;Newman et al 2003;Deser et al 2004;Schneider and Cornuelle 2005;Vimont 2005). On decadal timescales, the PDO is highly correlated with ENSO (Zhang and Church 2012) and the Interdecadal Pacific Oscillation (IPO), a basin-wide decadal climate mode associated with decadal SST variability in the Pacific (e.g., Power et al 1999;Folland et al 2002;Meehl and Hu 2006).…”
Section: Pdo-related Sea Level Patternsmentioning
confidence: 99%
“…The relationship of the PDO to ENSO outliers is shown in Figure 13 for two typical La Niña and El Niño cases. In general, there is an expectation that the PDO will have the same sign as the concurrent ENSO event (see the discussion by Newman et al (2003)). This situation partially prevails in Figure 13 and in other outlier cases examined.…”
Section: Large-scale Climatic Oscillationsmentioning
confidence: 99%
“…Movement of TCs is affected by both external (Neumann, 1992) and internal Williams, 1987, 1994) factors. George and Gray (1976) and Chan and 828 A. Z.-C. GOH AND J. C. L. CHAN Gray (1982) related the 500-hPa flow to the steering of TCs, while Ho et al (2004) and Lee et al (2006) both suggested the subtropical high as a steering factor.…”
Section: Introductionmentioning
confidence: 99%