Zonal and Vertical Structure of the Madden–Julian Oscillation

By G. Kiladis, K. Straub, P. Haertel. 2005

578 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/0239f3cd119ceabba09610db6468e4511d778247

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Citations in the corpus

Simulations of the Madden–Julian oscillation in four pairs of coupled and uncoupled global models (2006, background): “That is what suggested by global data assimilation products (e.g., Hendon and Salby 1994; Jones and Weare 1996; Maloney and Hartmann 1998; Sperber 2003; Kiladis et al 2005 ), GCM simulations (e.g., Kemball-Cook et al. 2002; Sperber et al. 2005), and the most popular MJO theories (e.g., Wang 1988; W”
Convectively coupled equatorial waves (2009, background): “Overall, ER wave structure varies much more substantially by season and regionally than the CCEWs treated so far (as does the MJO [Kiladis et al., 2005]), but Figure 17 is representative of ER structures over the warm pool in general.”
ENSO regulation of MJO teleconnection (2011, background): “Once the disturbances reach the dateline; thus, over cool equatorial waters, the convection demises and the disturbance is seen only in dynamical fields (Rui and Wang 1990; Hendon and Salby 1994; Matthews 2000; Sperber 2003; Kiladis et al. 2005).”
Observed Characteristics of the MJO Relative to Maximum Rainfall (2007, background): “In particular, the general characteristics and life cycle of the MJO as seen in a number of atmospheric variables have been researched (Hendon and Salby 1994; DeMott and Rutledge 1998; Maloney and Hartmann 1998; Myers and Waliser 2003; Kiladis et al. 2005, hereafter KSH05).”
A stochastic multicloud model for tropical convection (2010, background): “However, tropical convective systems have genuine multiscale and multiphysics dynamics in the sense that the larger scale features are not just a simple linear/rescaling transformation of the smaller scale features, unlike homogeneous turbulence, but they enjoy many dynamical differences as well [54”
Moist Static Energy Budget of MJO-like Disturbances in the Atmosphere of a Zonally Symmetric Aquaplanet (2012, background): “Much like observations of the Earth’s MJO, the observed anomalies have a tilted vertical structure (figure 6a), with preconditioning of the lower and middle troposphere ahead (east) of the convective signal (Kiladis et al. 2005).”
Structure of the Madden-Julian Oscillation in the Superparameterized CAM (2009, background): “Further discussion of GCM–CRM coupling can be found in Khairoutdinov and Randall (2003) and Khairoutdinov et al. (2005).”
The MJO as a Dispersive, Convectively Coupled Moisture Wave: Theory and Observations (2016, unknown): “…Based on the above discussion, this result indicates that westerlies from the Rossby wave response dominate the region of enhanced moisture and convection in the MJO, as was noted by Rui and Wang (1990), Hendon and Salby (1994), Kiladis et al. (2005), Adames and Wallace (2014b), among many others.”
Application of MJO Simulation Diagnostics to Climate Models (2009, background): “The equatorial vertical structure of the MJO has been examined in a number of studies (Rui and Wang 1990; Myers and Waliser; 2003; Sperber 2003; Kiladis et al. 2005; and Tian et al. 2006).”
Madden‐Julian Oscillation (2005, background): “Reconstruct the MJO from the leading modes and examine its primary features, such as the zonal scale, RG2003 Zhang: MADDEN-JULIAN OSCILLATION 15 of 36 RG2003 propagation speed, and structure [e.g., Sperber, 2003; Kiladis et al., 2005].”
A New Multiscale Model for the MaddenJulian Oscillation (2005, background): “Statistical composites of reanalysis data (Hendon and Salby 1994; Kiladis et al. 2005) give insight into the horizontal and vertical structure of the planetary-scale MJO envelope with crucial features documented such as quadrupole vortices in the horizontal flow field (Hendon and Salby 1994, Fig.”
Primary and successive events in the Madden–Julian Oscillation (2008, background): “There are positive temperature anomalies above, sloping upward towards the east, consistent with the analysis of Kiladis et al. (2005), and indicating eastward and upward propagation of a Kelvin wave.”
Structure and Properties of Madden–Julian Oscillations Deduced from DYNAMO Sounding Arrays (2013, background): “…envelope—cool anomalies at low levels and warm anomalies in the upper troposphere—are consistent with ﬁndings from past studies (Lin and Johnson 1996; Kiladis et al. 2005). d Tilted cool/warm and zonal wind anomalies oc-curred for extended periods (multiple weeks) in the upper troposphere and…”
A Simple Multicloud Parameterization for Convectively Coupled Tropical Waves. Part I: Linear Analysis (2006, background): “Recent analysis of observations over the warm pool in the Tropics reveals the ubiquity of three cloud types above the boundary layer: shallow congestus clouds, stratiform clouds, and deep penetrative cumulus clouds (Lin and Johnson 1996; Johnson et al. 1999).”
Fifty Years of Research on the Madden‐Julian Oscillation: Recent Progress, Challenges, and Perspectives (2020, background): “…of MJO convection is characterized by enhanced lower‐tropospheric moisture anomalies (e.g., Johnson & Ciesielski, 2013; Kemball‐Cook & Weare, 2001; Kiladis et al., 2005; Sperber, 2003; Tian et al., 2010), warm sea surface temperature (SST; Hendon & Glick, 1997; Woolnough et al., 2000; Shinoda…”
Three-Dimensional Structure and Dynamics of African Easterly Waves. Part I: Observations (2006, background): “9a, with the lower-level upward motion consistent with the maximum level of dynamical forcing, and the upper-level signal at around 300 hPa due to convective heating, as in other observed equatorial waves (e.g., Kiladis et al. 2005, and references therein).”
Tracking Pulses of the Madden–Julian Oscillation (2013, background): “This asymmetry in moisture variability associated with the MJO has been documented before (Kiladis et al. 2005).”