Suppose that the mean zonal wind shear in the descending westerlies of the equatorial QBO can be represented analytical...
Let some one who knows the answer completely answer this question. Suppose that the mean zonal wind shear in the descending westerlies of the equatorial QBO can be represented analytically on the equatorial B plane in the form au/dz exp (-2/L*) 1200 km. Determine the approximate meridional dependence of the corresponding temperature anomaly for lyl < where L =