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- W1649657864 abstract "Abstract Here we ask, what controls the horizontal scale of the Madden‐Julian Oscillation, i.e., what controls its zonal wave number k ? We present a new one‐dimensional (1D) β ‐plane model that successfully simulates the MJO with the same governing mechanism as the 2D shallow water model of Yang and Ingersoll (2013). Convection is parameterized as a short‐duration localized mass source that is triggered when the layer thickness falls below a critical value. Radiation is parameterized as a steady uniform mass sink. Both models tend toward a statistically steady state—a state of radiative‐convective equilibrium, not just on a global scale but also on the scale of each MJO event. This gives k ~ ( S c / c ) 1/2 , where S c is the spatial‐temporal frequency of convection events and c is the Kelvin wave speed. We offer this scaling as a prediction of how the MJO would respond to climate change." @default.
- W1649657864 created "2016-06-24" @default.
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- W1649657864 date "2014-02-07" @default.
- W1649657864 modified "2023-10-16" @default.
- W1649657864 title "A theory of the MJO horizontal scale" @default.
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- W1649657864 doi "https://doi.org/10.1002/2013gl058542" @default.
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