Summary
The environmental conditions in advance of three West African disturbance lines and three Eastern Atlantic squall lines are examined as is the modification of the environment during the passage of such storms over a site. A comparison with other tropical squall lines observed over Venezuela is made. A model of the relative airflow within a West African disturbance line is presented and some aspects of storm movement are considered. The hydraulic jump analogy and a density current model are applied to the convective systems and the results obtained are compared with observations. The hydraulic jump analogy gives reasonable predictions for the storms' speeds and the density current model results show that for the West African disturbance lines, as well as the Venezuelan storms, a close relationship exists between the storm speed and the speed of the density current. As this relationship is not observed in the Eastern Atlantic squall lines, it appears that the density current model is not applicable to convective systems occurring over the ocean.
Zusammenfassung
Es werden die Verhältnisse im Bereich von drei sich annähernden westafrikanischen Störungslinien und von drei ostatlantischen Böenlinien wie auch die Modifikation der Umgebung beim Durchzug solcher Störungen untersucht. Ein Vergleich mit anderen über Venezuela beobachteten tropischen Böenlinien wird gemacht. Ein Modell der relativen Luftströmung in einer westafrikanischen Störungslinie wird dargelegt und einige Aspekte der Bewegung der Störung werden in Betracht gezogen. Die hydraulische Jump-Analogie und ein Dichtestrom-Modell werden auf konvektive Systeme angewendet und die Ergebnisse werden mit Beobachtungen verglichen. Die hydraulische Jump-Analogie gibt vernünftige Vorhersagen für die Störungsgeschwindigkeiten, und das Dichtestrom-Modell zeigt das Ergebnis, daß sowohl bei westafrikanischen Störungslinien wie auch bei den Störungen in Venezuela eine enge Beziehung zwischen der Störungsgeschwindigkeit und der Geschwindigkeit des Dichtestromes besteht. Da diese Beziehung nicht bei ostatlantischen Böenlinien beobachtet wird, scheint es, daß das Dichtestrom-Modell auf konvektive Systeme über dem Ozean nicht anwendbar ist.
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Fernandez, W. Environmental conditions and structure of the West African and Eastern Tropical Atlantic squall lines. Arch. Met. Geoph. Biocl. A. 31, 71–89 (1982). https://doi.org/10.1007/BF02257743
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DOI: https://doi.org/10.1007/BF02257743