Summary
A time cross-section was constructed for Cairo during the period 10–31 Dec. 57. The outstanding feature of this cross-section is the periodic existence of high wind maxima associated with high cloud formation. A method was suggested for the location of high wind centers from the thermal field only. Moreover, the climatological means of high clouds showed quick changes in the period of the Jet Stream migration. This has been taken as an evidence of the relation between the subtropical Jet Stream and high cloud formation in the region.
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Eltantawy, A.I. Jet stream clouds in the Middle East. Geofisica Pura e Applicata 46, 352–359 (1960). https://doi.org/10.1007/BF02001115
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DOI: https://doi.org/10.1007/BF02001115