EOF Representations of the Madden–Julian Oscillation and Its Connection with ENSO*

By W. Kessler. 2001

248 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/b20fe4eb5aac1802d90aeb0819bfe008056ea735

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Citations in the corpus

Changes in the Activity of the Madden–Julian Oscillation during 1958–2004 (2006, methodology): “Kessler (2001) pointed out that the third EOF has a maximum in the region 150°E–170°W, and the phasing between the first and third EOFs is such that during warm ENSO events, EOF3 weakens EOF1 in the Indian Ocean and strengthens EOF1 in the Pacific, which better characterizes the propagation of MJO…”
A Comparison of OLR and Circulation-Based Indices for Tracking the MJO (2014, methodology): “2012), or latitudinally averaged OLR data have been used as the EOF basis, while choosing a range in latitude such as 158S–158N that spans the full seasonal migration of the MJO (Maloney and Hartmann 1998; Kessler 2001).”
An All-Season Real-Time Multivariate MJO Index: Development of an Index for Monitoring and Prediction (2004, unknown): “In the analysis chosen for our index deﬁnition, near-equatorially averaged (15 (cid:56) S– 15 (cid:56) N) ﬁelds are used, like Maloney and Hartmann (1998) and Kessler (2001).”
The global response to tropical heating in the Madden–Julian oscillation during the northern winter (2004, background): “During El Ni~no events, observed MJO convective anomalies tend to propagate further eastward than usual, into the central Paci c (Kessler 2001).”
A Comparison of the Influence of Additive and Multiplicative Stochastic Forcing on a Coupled Model of ENSO (2005, background): “While this is a rather controversial topic and an area of intense research, Kessler (2001) noted that it is not the global aspects of the MJO that are related to ENSO, but rather the meandering over the Pacific Ocean of the winds associated with the MJO that is related to ENSO’s interannual…”
Influence of the Madden–Julian Oscillation on East African rainfall: II. March–May season extremes and interannual variability (2006, background): “Positive (negative) significant correlations (Bravais–Pearson test, 95% level) are contoured with solid (dashed) lines. by Slingo et al. (1999) and Kessler (2001)) it is suggested by Kessler that the MJO is less active over the Indian Ocean during the height of warm ENSO events—and more active over…”
MJO simulation in CMIP5 climate models: MJO skill metrics and process-oriented diagnosis (2017, unknown): “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”
MJO Initiation in the Real-Time Multivariate MJO Index (2013, background): “…1992; Hendon and Salby 1994; Hendon et al. 1999; Matthews and Kiladis 1999; Matthews 2000;Wheeler et al. 2000; Kemball-Cook and Weare 2001; Kessler 2001; Myers and Waliser 2003; Kiladis et al. 2005; Benedict and Randall 2007; Matthews 2008; Kiladis et al. 2009); 2) Dynamical- or…”
Madden‐Julian Oscillation (2005, background): “…possible feedback between the MJO and ENSO SST is manifested by the observed correlation between the local MJO in the Pacific and ENSO SST indices [Kessler, 2001], in contrast to the interannual variability of the global MJO that is independent of ENSO SST [Slingo et al., 1999; Hendon et al.,…”
Atmosphere‐ocean coupled processes in the Madden‐Julian oscillation (2015, background): “The prominence of intraseasonal convective variability over the Indian and western Pacific Oceans was noted during the earliest stages of MJO research, but the possibility that air-sea interactions could provide an energy source to convective motions that are sustained for 30–50 day periods was not ”
Evolution of the 2002/03 El Niño* (2003, background): “Are these yearly differences in the statistics of episodic westerly wind events and the MJO controlled by random variations in internal atmospheric dynamics, by underlying interannual Indo-Pacific SST variations, or by a combination of these factors (e.g., Hendon et al. 1999; Kessler 2001)?”
An Indian monsoon intraseasonal oscillations (MISO) index for real time monitoring and forecast verification (2013, background): “…Institute for Regional Earth System Science and Engineering, University of California Los Angeles, Los Angeles, California 90095, USA B. N. Goswami Indian Institute of Tropical Meteorology, Dr. Homi Bhaba Road, Pashan, Pune 411008, India (Lau and Chan 1985; Maloney and Hartmann 1998; Kessler 2001).”
ENSO regulation of MJO teleconnection (2011, background): “However, during mature phases of El Niño events the MJO activity markedly shifts eastward into the central Pacific, expanding the longitudinal domain of the MJO convective activity (Fink and Speth 1997; Hendon et al. 1999; Kessler 2001).”
The Tropical Subseasonal Variability Simulated in the NASA GISS General Circulation Model (2012, background): “…summer monsoons (e.g., Yasunari 1979; Wheeler and McBride 2005), the formation of TCs (e.g., Liebmann et al. 1994; Maloney and Hartmann 2000b,a; Bessafi and Wheeler 2006; Camargo et al. 2009), and the onset of some El Niño events (e.g., Takayabu et al. 1999; Bergman et al. 2001; Kessler 2001).”
The ``Year'' of Tropical Convection (May 2008-April 2010): Climate Variability and Weather Highlights (2012, background): “…the spatial characteristics and manifestations of intraseasonal variability (e.g., MJO) can be modified by the conditions of ENSO and the Indian Ocean dipole (e.g., Hendon et al. 1999; Kessler 2001; Waliser et al. 2001; Lau 2005; Hendon et al. 2007; Rao et al. 2007; Ajayamohan et al. 2009).”