Cranica wrote:That's some pretty worrisome TCHP in the Caribbean as we go into October - what's odd is that the SSTs are near-normal, but the TCHP is ridiculously high.
Any of the pro mets around know why we keep getting these insanely vigorous, well-organized waves, despite the Atlantic being so hostile? It seems weird that they keep coming off the Sahara so healthy, then fizzle in the open Atlantic.
The West African Monsoon system is fairly robust year in and year out (mainly due to strong temperature gradient between Sahara and Gulf of Guinea), so the African Easterly Jet is always propagating African Easterly Waves (AEWs) toward the west coast of North Africa. Further east, topography such as the Ethiopian Highlands and the Darfur Mountains help to initiate convection as the flow is forced up and over these features. The jet takes care of delivering these disturbances to the east Atlantic while the waves grow via baroclinic and barotropic energy conversions. There is some debate about how important the wave initiation between Darfur and Ethiopia is compared to the wave maintenance via the jet. However, you can count on a wave exiting the African coast about every 2 days. Waves that exit the African coast exhibit intraseasonal variability (i.e. - the frequency, strength, etc. varies within the summer season), which is why we get periods of strong AEWs and periods of not-so-strong AEWs. Also, these waves do not come from the Sahara. They need the moisture of the Sahel and further south in order to thrive. Hope this helps!