Models for Tropical Climate Dynamics by Boualem Khouider

Author:Boualem Khouider
Language: eng
Format: epub
ISBN: 9783030177751
Publisher: Springer International Publishing

where the indices refer to the first and third baroclinic modes. As such it serves both as a measure for the vertical shear strength and to set the lag between the stratiform anvils and the organized convection core, which determines the imposed tilt.

Here V ∗ sets a threshold beyond which mesoscale organization becomes significant. When V T << V ∗, CMT is downscale; we have essentially turbulent dissipation through dry eddies or cumulus friction due to upright convection, and when V T >> V ∗ upscale mesoscale CMT becomes dominant.

Similarly to the precedent model, the velocity perturbations v ′, w ′ are obtained in closed form from WTG approximation,

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