Moisture Modes and the Madden–Julian Oscillation

Moisture mode instability is thought to occur in the tropical oceanic atmosphere when precipitation is a strongly increasing function of saturation fraction (precipitable water divided by saturated precipitable water) and when convection acts to increase the saturation fraction. A highly simplified...

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Veröffentlicht in:	Journal of climate 2009-06, Vol.22 (11), p.3031-3046
Hauptverfasser:	Raymond, David J., Fuchs, Željka
Format:	Artikel
Sprache:	eng
Schlagworte:	Advection Atmosphere Atmospheric models Atmospheric moisture Climate models Climate system Climatology. Bioclimatology. Climate change Convection Data collection Dynamical systems Earth, ocean, space Entropy Exact sciences and technology External geophysics Meteorology Parameterization Precipitation Rain Saturation Scale models Sea surface temperature Simulations Toy models Tropical environments Velocity
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