Rectification of the Madden-Julian Oscillation into the ENSO Cycle.

By W. Kessler, Richard Kleeman. 2000

330 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/7573319ae195d02072928b22845ba8bab03a063e

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Atmospheric Science

In Global and Planetary Change

In Oceanography

Citations in the corpus

A Comparison of the Influence of Additive and Multiplicative Stochastic Forcing on a Coupled Model of ENSO (2005, methodology): “Most previous studies of ENSO as a stochastically forced oscillation have focused primarily on additive stochastic forcing (i.e., forcing that is independent of ENSO amplitude and phase; Eckert and Latif 1997; Kleeman and Moore 1997; Moore and Kleeman 1999a; Penland 1996; Penland and Matrasova 1994;”
Evolution of the 2002/03 El Niño* (2003, background): “Plausible physical mechanisms by which higher-frequency dynamics associated with the MJO can influence ENSO have been described (Kessler et al. 1995; Kessler and Kleeman 2000; Bergman et al. 2001; Zhang 2001).”
Climate Fluctuations of Tropical Coupled Systems—The Role of Ocean Dynamics (2006, background): “All noise forcing is not equal, however, and the spatial structure of some types of high-frequency atmospheric phenomena may project especially well onto optimally growing perturbations (Kessler and Kleeman 2000; Moore and Kleeman 1999b).”
ENSO regulation of MJO teleconnection (2011, background): “Southern Oscillation (ENSO) is the most energetic and predictable mode of the global climate system, and its relation with the MJO has been extensively studied (Lau and Chan 1988; Lau and Shen 1988; Weickmann 1991; Takayabu et al. 1999; Kessler and Kleeman 2000; Bergman et al. 2001; Zhang and Gott”
MJO prediction in the NCEP Climate Forecast System version 2 (2014, background): “The MJO also affects the variability and prediction of the climate at longer time scales such as the El Nino Southern Oscillation (ENSO) (Kessler and Kleeman 2000; Wang et al. 2011).”
The response of the coupled tropical ocean–atmosphere to westerly wind bursts (2002, background): “A study of the recti ed effect on the ocean of a sequence of alternating EWBs and WWBs has been completed by Kessler and Kleeman (2000).”
Fifty Years of Research on the Madden‐Julian Oscillation: Recent Progress, Challenges, and Perspectives (2020, background): “…MJO also interacts with other prominent modes of climate variability, including the El Niño/Southern Oscillation (ENSO; e.g., Hendon et al., 2007; Kessler & Kleeman, 2000; McPhaden, 1999; Takayabu et al., 1999), Arctic Oscillation (AO; L'Heureux & Higgins, 2008), North Atlantic Oscillation (NAO;…”
A simple approach to quantifying the noise–ENSO interaction. Part I: deducing the state-dependency of the windstress forcing using monthly mean data (2015, background): “Therefore, it has been suggested that these WWBs are not just a forcing mechanism for ENSO but are also affected by the underlying state of ENSO, and potentially a multiplicative noise process (Kessler and Kleeman 2000; Vecchi and Harrison 2000; Yu et al. 2003; Eisenman et al. 2005; Perez et al. 200”
MJO simulation in CMIP5 climate models: MJO skill metrics and process-oriented diagnosis (2017, neutral): “The MJO interacts with a wide range of tropical weather and climate phenomena that include the onset and break of monsoons (Yasunari 1979, 1980; Lau and Chan 1986; Hendon and Liebmann 1990; Sperber et al. 2000; Sultan et al. 2003; Annamalai and Sperber 2005; Wheeler and McBride 2005; Lorenz and Hart”
EOF Representations of the Madden–Julian Oscillation and Its Connection with ENSO* (2001, background): “Its maximum is found in the region of 1508E–1708W, in the west Pacific warm pool where mechanisms proposed for MJO–ENSO interaction occur (e.g., Kessler and Kleeman 2000).”
Evaluation of MJO Forecast Skill from Several Statistical and Dynamical forecast Models (2009, background): “structure in the equatorial Pacific Ocean via downwelling oceanic Kelvin waves and the wave activity impacts the overall intensity of El Niño episodes (McPhaden 1999, 2004; Kessler and Kleeman 2000; Zhang and Gottschalck 2002; Seo and Xue 2005).”
Madden‐Julian Oscillation (2005, background): “Mean SST in the western Pacific can be reduced by net cooling due to the MJO [e.g., Kessler and Kleeman, 2000; Shinoda and Hendon, 2002].”
Understanding Enso Physics—A Review (2013, background): “Some studies have argued that ISV does not play a critical role in ENSO [e.g., Zebiak, 1989b; Slingo et al., 1999; Syu and Neelin, 2000; Kessler and Kleeman, 2000].”