Tropical Pacific Decadal Variability and Its Relation to Decadal Modulations of ENSO

By K. Rodgers, Petra Friederichs, M. Latif. 2004

266 citations recorded by the source corpus.

Subfields: Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/3974de47fcd88bdeb59ae3f6ecff64f1c10cfe4e

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In Global and Planetary Change

In Oceanography

Citations in the corpus

El Niño Modoki and its possible teleconnection (2007, background): “This asymmetry (Rodgers et al., 2004; An and Jinn, 2004) per se, however, can not result in ENSO Modoki owing to the reason that both El Niño and La Niña do not occur simultaneously.”
ENSO Modulation: Is It Decadally Predictable? (2014, background): “The predictability of ENSO modulation bears not only on prospects for decadal forecasts of ENSO but also on decadal predictability of other phenomena— ENSO modulation is known to rectify into decadal and longer time scales (Fl€ ugel and Chang 1999; Newman et al. 2003; Rodgers et al. 2004; An 2004; Y”
The eastward shift of the Walker Circulation in response to global warming and its relationship to ENSO variability (2014, background): “Another important feature of ENSO variability is its spatial asymmetry (e.g. Hoerling et al. 1997; Rodgers et al. 2004; Yu and Kim 2011; Dommenget et al. 2013), i.e. that the warming of SST during El Niño events occurs further to the east than the SST cooling during La Niña events.”
Analysis of the non-linearity in the pattern and time evolution of El Niño southern oscillation (2013, background): “However, it has also been noted that observed and simulated ENSO events can have different patterns, in particular it has been pointed out that El Niño events are different in pattern from La Niña events (e.g. Hoerling et al. 1997; Monahan 2001; Rodgers et al. 2004; Schopf and Burgman 2006; Sun and ”
The Effect of Orbital Forcing on the Mean Climate and Variability of the Tropical Pacific (2007, unknown): “Despite the fact that ENSO variability is highly skewed in the ECHO-G simulation (Rodgers et al. 2004), the background state rectification due to ENSO variance changes (Clement et al. 1999) does not seem to play a major role.”
Warm Pool and Cold Tongue El Nino Events as Simulated by the GFDL 2.1 Coupled GCM (2010, background): “First, the WP El Niño could be inducing the tropical decadal variability by means of a nonlinear rectification effect (Timmermann 2003; Rodgers et al. 2004; An et al. 2005; An 2009).”