An Idealized Semi-Empirical Framework for Modeling the Madden–Julian Oscillation
By A. Sobel, E. Maloney. 2012
270 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/0c3720e8c070ff6a9a78c4403c03696c0aeff3e4
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Citations in the corpus
- Global‐scale convective aggregation: Implications for the Madden‐Julian Oscillation (2015, background): “…prerequisite for realistic MJO simulation [e.g., Wang and Schlesinger, 1999; Thayer-Calder and Randall, 2009], and simple theoretical models of the MJO often rely on the assumption that precipitation is a strong function of water vapor [e.g., Fuchs and Raymond, 2002; Sobel and Maloney, 2012].”
- Fifty Years of Research on the Madden‐Julian Oscillation: Recent Progress, Challenges, and Perspectives (2020, methodology): “It is hypothesized that the GMS should be small or negative in order to sustain strong MJO convection (Benedict et al., 2014; Hannah & Maloney, 2011; Inoue & Back, 2015a; Raymond et al., 2009; Raymond & Fuchs, 2009; Sobel & Maloney, 2012).”
- Self‐aggregation of convection in long channel geometry (2014, unknown): “If such an instability indeed exists in the real atmosphere, it would reshape our understanding of tropical circulations and could help to explain the growth and life cycle of large-scale organized convective systems such as tropical cyclones and the Madden–Julian Oscillation (e.g. Bretherton et al.”
- Prediction of the Madden–Julian Oscillation: A Review (2018, background): “From the moisture mode theory view (e.g., Raymond and Fuchs 2009; Sobel and Maloney 2012, 2013; Adames and Kim 2016), it has been argued that the horizontal moisture advection tends to play a dominant role in the eastward propagation of the MJO through the Maritime Continent.”