A New Model of the Madden–Julian Oscillation

By D. Raymond. 2001

283 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/2af85ebd97f349a38514054c231073f7b92121e5

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Citations in the corpus

Zonal and Vertical Structure of the Madden–Julian Oscillation (2005, background): “…responsible for the coupling of convection to the large-scale MJO circulation, while other simulations have provided insight into the potential roles of air–sea interaction (e.g., Emanuel 1987; Neelin et al. 1987) and cloud-radiation feedback (Hu and Randall 1994; Raymond 2001) in the MJO.”
Surface Fluxes and Tropical Intraseasonal Variability: a Reassessment (2008, background): “In extratropical atmospheric dynamics it has proved extremely useful to separate dry adiabatic dynamical mechanisms (e.g., Hoskins et al. 1985) from those in which ‘‘diabatic’’ processes (defined for a dry working fluid with phase changes of water considered external), which break the conservation…”
The Role of Convective Moistening in the Madden–Julian Oscillation (2009, background): “Raymond (2001) proposes that the oscillations are maintained by a surface-flux feedback in which convection leads to convergence near the surface, which produces stronger surface fluxes, that then reduce the column saturation deficit.”
Intraseasonal Variability in an Aquaplanet General Circulation Model (2010, methodology): “The structure of the MJO in this model resembles the moisture mode in the b-plane tropical channel model of Raymond (2001) and follow-up papers (e.g. Raymond 2007), consisting of a strong offequatorial cyclonic gyre bounded on its equatorial side by a strong jet exceeding 10 m s21, with…”
Fifty Years of Research on the Madden‐Julian Oscillation: Recent Progress, Challenges, and Perspectives (2020, background): “The first studies indicating that theMJOmay be a moisture mode were Raymond (2001) and Sobel et al. (2001).”
Systematic Multiscale Models for the Tropics (2003, background): “Despite substantial theoretical efforts, the mechanisms for the tropical intraseasonal oscillation remain to be elucidated (Raymond 2001, and references therein), while many aspects Corresponding author address: Prof. Andrew J. Majda, Courant Institute of Mathematical Sciences, New York University,…”
Atmosphere‐ocean coupled processes in the Madden‐Julian oscillation (2015, background): “The drawbacks to satellite flux data sets are their limited temporal record (∼1987 onward) and the remaining challenge of retrieving near-surface air temperature and humidity [Schulz et al., 1993; Jin and Yu, 2015], although progress is being made [e.g., Jackson et al., 2006; Jackson and Wick,…”
On the Role of Moist Processes in Tropical Intraseasonal Variability: Cloud–Radiation and Moisture–Convection Feedbacks (2005, background): “…moisture (water vapor, clouds) and on their potential role in the organization of tropical convection through radiative and convective feedbacks (Raymond 2001; Tompkins 2001; Fuchs and Raymond 2002; Myers and Waliser 2003; Sperber 2003; Grabowski 2003; Grabowski and Moncrieff 2004, hereafter…”
Analytic representation of the large-scale organization of tropical convection (2004, background): “Raymond (2001) argues the significance of cloud radiation and that the intraseasonal oscillation is mainly a balanced (Rossby) response to parameterized heating.”
Tracking Pulses of the Madden–Julian Oscillation (2013, background): “Hypothesis I is built upon the abundant literature on the sensitivity of convection to environmental moisture (Brown and Zhang 1997; Raymond 2001; Kuang and Bretherton 2006; Peters and Neelin 2006).”
Madden‐Julian Oscillation (2005, methodology): “tion selectively to the intraseasonal, planetary-scale, and slowly eastward propagating disturbances known as the MJO? The MJO can be regarded as the ‘‘holy grail’’ of the tropical atmospheric dynamics [Raymond, 2001], and it has motivated many hypotheses describing potential roles of certain physic”