THE MECHANISM OF THE DEVELOPMENT OF THE RED SEA CONVERGENCE ZONE

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LASHKARI H.

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Journal: GEOGRAPHICAL RESEARCH Year:2001 | Volume:15 | Issue:3-4 (58-59) Page(s): 167-184

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Information Journal Paper

Title

THE MECHANISM OF THE DEVELOPMENT OF THE RED SEA CONVERGENCE ZONE

Author(s)

LASHKARI H. | Issue Writer Certificate

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Abstract

Special attention should be paid to the topographical condition of the Red Sea coastal areas, particularly in the northern half of the sea where mountain ranges that surround the sea almost touch the water. Consequently, in the cold half of the year, synoptic systems of the region result in producing S-SE current in the southern half and N-NE currents in the northern half. These currents that blowing the opposite direction and face each other around the area limited approximately between 18°-22°where they create a noticeable convergence zone.Concurrently, when the North African trough develops over Egypt and the Sudan, the Red Sea convergence zone is highly activated and causes the trough to move east under the convergence zone causing unusually heavy rainfall over the south and south east Iran

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APA: Copy

LASHKARI, H.. (2001). THE MECHANISM OF THE DEVELOPMENT OF THE RED SEA CONVERGENCE ZONE. GEOGRAPHICAL RESEARCH, 15(3-4 (58-59)), 167-184. SID. https://sid.ir/paper/29766/en

Vancouver: Copy

LASHKARI H.. THE MECHANISM OF THE DEVELOPMENT OF THE RED SEA CONVERGENCE ZONE. GEOGRAPHICAL RESEARCH[Internet]. 2001;15(3-4 (58-59)):167-184. Available from: https://sid.ir/paper/29766/en

IEEE: Copy

H. LASHKARI, “THE MECHANISM OF THE DEVELOPMENT OF THE RED SEA CONVERGENCE ZONE,” GEOGRAPHICAL RESEARCH, vol. 15, no. 3-4 (58-59), pp. 167–184, 2001, [Online]. Available: https://sid.ir/paper/29766/en

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