Abstract
Spectrum and cross-spectrum analysis are used to determine the source region of the waves observed during the period 23 August-19 September 1974. It is proposed that the large wave growth in the region between 0 and 10oE was caused by a combination of 2 factors: the increased instability of the mid-tropospheric easterly jet in that region, and the better organization of the convection by the enhanced waves allowing condensation heating also to contribute to their growth.-from Authors
Cite
CITATION STYLE
Albignat, J. P., & Reed, R. J. (1980). The origin of African wave disturbances during Phase III of GATE. Monthly Weather Review, 108(11), 1827–1839. https://doi.org/10.1175/1520-0493(1980)108<1827:TOOAWD>2.0.CO;2
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