A Systematic Comparison of Tropical Waves over Northern Africa. Part II: Dynamics and Thermodynamics

This study presents the first systematic comparison of the dynamics and thermodynamics associated with all
major tropical wave types causing rainfall modulation over northern tropical Africa: the Madden–Julian
oscillation (MJO), equatorial Rossby waves (ERs), tropical disturbances (TDs, including African easterly
waves), Kelvin waves, mixed Rossby–gravity waves (MRGs), and eastward inertio-gravity waves (EIGs).
Reanalysis and radiosonde data were analyzed for the period 1981–2013 based on space–time filtering of
outgoing longwave radiation. The identified circulation patterns are largely consistent with theory. The slow
modes, MJO and ER, mainly impact precipitable water, whereas the faster TDs, Kelvin waves, and MRGs
primarily modulate moisture convergence. Monsoonal inflow intensifies during wet phases of the MJO, ERs,
and MRGs, associated with a northward shift of the intertropical discontinuity for MJO and ERs. This study
reveals that MRGs over Africa have a distinct dynamical structure that differs significantly from AEWs.
During passages of vertically tilted imbalanced wave modes, such as the MJO, TDs, Kelvin waves, and partly
... mehr
MRG waves, increased vertical wind shear and improved conditions for up- and downdrafts facilitate the
organization of mesoscale convective systems. The balanced ERs are not tilted, and rainfall is triggered by
large-scale moistening and stratiform lifting. The MJO and ERs interact with intraseasonal variations of the
Indian monsoon and extratropical Rossby wave trains. The latter causes a trough over the Atlas Mountains
associated with a tropical plume and rainfall over the Sahara. The presented results unveil which dynamical
processes need to be modeled realistically to represent the coupling between tropical waves and rainfall in
northern tropical Africa