Answers are grounded in this paper and cite their sources.
The nature of African easterly waves (AEWs) and the easterly wave season over West Africa are examined using the National Centers for Environmental Prediction (NCEP) reanalysis. The study is carried out with two objectives in mind. The first goal is to describe the seasonal cycle of wave activity and to determine if it has a distinctive signature. To achieve this, the temporal evolution of wave period, amplitude, and structure are examined with wavelet analysis. This analysis is carried out at a grid point (158N, 08) that is at located where AEWs are well developed. The second goal is to determine differences in the wave characteristics and the wave season between wet and dry years. Regarding the seasonal cycle, it was found, in accordance with previous research, that AEW activity typically occurs between May and October. Disturbances have a periodicity between 4 and 8 days. At the level (600 mb) of the African easterly jet (AEJ) there was a broad peak in the magnitude of the variance over the months of July, August, and September. This may be due to the increased horizontal shear and barotropic instability, which also peaks at that time. There is a greater contribution of variance from longer periods (6.25–7.5 days) in the later half of the summer. At lower levels, the disturbances appear to be confined to periods of 3.75–5.0 days, with the maximum variance in the mean occurring in July. This may be a response to the change in the magnitude
No takes yet. Share an insight, caveat, or question.
Jeremy P. Grist (2002) studied this question.
Synapse has enriched 10 related papers. Consider them for comparative context: