17th Conference on Atmospheric and Oceanic Fluid Dynamics

13.1

Convectively-coupled gravity waves in the tropics

Stefan N. Tulich, CIRES/Univ. of Colorado, Boulder, CO; and G. Kiladis

Observations are presented showing evidence for a strong, two-way coupling between tropical convection and zonally-propagating gravity wave disturbances with periods < 2 days and zonal scales < 1000 km. To address the question of why westward-moving waves are seemingly preferred over eastward-moving, we describe results from explicit three-dimensional simulations of convection on an equatorial beta-plane, both with and without vertical shear of the background zonal flow.

wrf recording  Recorded presentation

Session 13, Interactions Between Tropical Convection and the Large Scale Circulation II
Friday, 12 June 2009, 8:00 AM-10:00 AM, Pinnacle BC

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