ENSO-Forced Variability of the Pacific Decadal Oscillation

By Matthew Newman, Gilbert P. Compo, M. Alexander. 2003

741 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/f017abb05711b08c558010a04679e6f78ce5e5b1

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Citations in the corpus

Recent trends in paralytic shellfish toxins in Puget Sound, relationships to climate, and capacity for prediction of toxic events (2009, background): “Essentially, this reflects the tendency for individual ENSO events to begin in one summer, peak the following winter, and then fade away in the subsequent spring (see Newman et al., 2003).”
Decadal variations of intense typhoon occurrence in the western North Pacific (2008, background): “It has been suggested that on a decadal time scale, the conditions in the North Pacific may be a ‘reddened’ response to ENSO (e.g. Newman et al. 2003).”
Regional relationships between climate and wildfire-burned area in the interior West, USA (2006, background): “One explanation for the differential effect of El Collins et al. Nifio and La Niiia on bumed area during warm-versus coolphase PDO lies in the fact that ENS0 may force PDO fluctuations (Newman et al. 2003).”
The Forcing of the Pacific Decadal Oscillation (2005, methodology): “This coefficient is about half the size of that obtained by Newman et al. (2003) .”
Regime shifts and red noise in the North Pacific (2006, background): “There is multi-year variation in the frequency of ENSO events which might also force an AR1 ocean process (Newman et al., 2003).”
Atmospheric bridge, oceanic tunnel, and global climatic teleconnections (2007, background): “…at decadal timescales [Trenberth, 1990; Graham et al., 1994; Deser et al., 2004b] or by ENSO-related forcing on interannual timescales, which is subsequently integrated, or ‘‘reddened,’’ by ocean processes including the reemergence mechanism [Newman et al., 2003; Schneider and Cornuelle, 2005].”
Feedbacks, Timescales, and Seeing Red (2009, background): “…of wintertime heat anomalies into the following year's mixed layer provides a consistent explanation for the near annual timescale of the memory, and Newman et al. (2003) have shown additional skill in explaining the PDO if an index of the El Niño Southern Oscillation is included as part of the…”
Sea surface temperature variability: patterns and mechanisms. (2010, background): “Examples include: SST fluctuations in the Southern Ocean associated with the Southern Annular Mode; a tri-polar pattern of SST anomalies in the North Atlantic associated with the North Atlantic Oscillation; and a pan-Pacific mode known as the Pacific Decadal Oscillation.”
Towards multi-resolution global climate modeling with ECHAM6–FESOM. Part I: model formulation and mean climate (2015, background): “This has also been suggested by Pierce (2001) and Newman et al. (2003), the latter of which interpret the PDO as a slow AR(1)-process that is driven by quasi random forcing by ENSO.”
Decadal Variability in the Kuroshio–Oyashio Extension Simulated in an Eddy-Resolving OGCM (2006, background): “1999) and its role in the decadal variability has been pointed out (Deser et al. 2002; Newman et al. 2003), the present study suggests that the re-emergence of subsurface thermal anomalies can also occur due to decadal-scale migration of a frontal axis and associated thermocline changes in associati”
Climate controls on marine ecosystems and fish populations (2010, background): “The PDO has been described as either a long-lived El Niño-like pattern of Indo-Pacific climate variability or a low frequency residual of ENSO variability on multi-decadal time scales (Newman et al., 2003).”
ENSO and meridional modes: A null hypothesis for Pacific climate variability (2015, positive): “For example, while eastern Pacific ENSO teleconnections preferentially energize the PDO pattern [e.g., Alexander et al., 2002; Newman et al., 2003; Deser et al., 2004], central Pacific ENSO events project onto the NPGO [e.”